arctic_proposals_from_gotw_summary_list_feb2011_for_website
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Award Title Investigator
Arctic hydrate dissociation as a consequence Professor T Minshull
of climate change: determining the
vulnerable methane reservoir and gas
escape mechanisms
Arctic hydrate dissociation as a consequence Dr M Ellis
of climate change: determining the
vulnerable methane reservoir and gas
escape mechanisms
Ocean Acidification Impacts on Sea-Surface Dr REM Rickaby
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Dr RJG Leakey
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Professor P Burkill
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Professor J Sharples
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Professor C Brownlee
Biology, Biogeochemistry and Climate
The spin-up of the Arctic Ocean Dr KA Giles
Networks of Sensors in Extreme Professor T Murray
Environments: High-Resolution Glacier
Dynamic Monitoring
Export of Ozone and Precursors from Europe Dr SR Arnold
and Impacts on Air Quality, Climate and
Ecosystems
Snow-Vegetation-Atmosphere Interactions Dr RLH Essery
over Heterogeneous Landscapes
An Aircraft-Deployable GPS Stake Network Dr G Gudmundsson
for Antarctic Glaciers
Development of a Miniature Static Imaging Dr TJ Nightingale
Fourier Transform Spectrometer (SIFTS)
Pan-Arctic Acoustic Archives: Quantifying Dr FR Cottier
zooplankton behaviours in a changing Arctic
Airborne geophysical investigations of basal Professor J Bamber
conditions at flow transitions of outlet
glaciers on the Greenland Ice Sheet
Airborne geophysical investigations of basal Professor MJ Siegert
conditions at flow transitions of outlet
glaciers on the Greenland Ice Sheet
Ocean Acidification Impacts on Sea-Surface Dr DJ Suggett
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Dr D.C.E. Bakker
Biology, Biogeochemistry and Climate
CO2-CarbonCycle-Climate-Interactions (C4I) Dr A Ridgwell
Ocean Acidification Impacts on Sea-Surface Dr PD Nightingale
Biology, Biogeochemistry and Climate
Ocean Acidification Impacts on Sea-Surface Dr R Sanders
Biology, Biogeochemistry and Climate
Airborne geophysical investigations of basal Professor JA Dowdeswell
conditions at flow transitions of outlet
glaciers on the Greenland Ice Sheet
Observations and synthesis to establish Professor A Watson
variability and trends of oceanic pH
Ocean and sea-ice dynamics in Nares Strait Dr HL Johnson
and the Canadian Arctic Archipelago
Ocean Acidification Impacts on Sea-Surface Dr T Tyrrell
Biology, Biogeochemistry and Climate
Investigating meltwater flow beneath the Dr A Hubbard
Greenland Ice Sheet using a multi-tracer
approach
Quantifying the population-level cost of Dr MC Fisher
amphibian chytridiomycosis in a changing
montane ecosystem
Field-ready phase-sensitive radio- Professor P Brennan
echosounder, for ice shelf melt rate
measurement
Oxbow Persistence as Aquatic Floodplain Dr J A Constantine
Habitat: Deciphering the Processes
Responsible for the Initial Open-Water
Volume Inherited by Oxbow Lakes
Snow-Vegetation-Atmosphere Interactions Dr NJ Rutter
over Heterogeneous Landscapes
Snow-Vegetation-Atmosphere Interactions Professor B Huntley
over Heterogeneous Landscapes
Understanding the Arctic continental shelf Dr Y Lenn
mixing regimes and their impact on shelf sea-
circulation and upper ocean stratification
A century of variability in Greenland melting Dr R Marsh
and iceberg calving
A century of variability in Greenland melting Professor GR Bigg
and iceberg calving
Observations and synthesis to establish Dr NJ Hardman-Mountford
variability and trends of oceanic pH
Investigating meltwater flow beneath the Dr PW Nienow
Greenland Ice Sheet using a multi-tracer
approach
Investigating meltwater flow beneath the Dr JL wadham
Greenland Ice Sheet using a multi-tracer
approach
IRD heavy minerals as a provenance tool for Dr CD Storey
ice coverage on Greenland
ASCOS Analysis - surface-cloud coupling in Dr IM Brooks
the arctic boundary layer
Are tropical uplands regional hotspots for Dr Y Teh
methane and nitrous oxide?
Interaction of Tectonics and Magmatism in Professor RS White
the Askja spreading segment of Iceland
Cryo-Egg: enabling wireless communications Dr JL wadham
for a deep subglacial application
Are tropical uplands regional hotspots for Professor P Meir
methane and nitrous oxide?
Mapping and sampling of the tephra fallout Dr TT Thordarson
from the 14 April - ongoing eruption at
Eyjafjoll volcano, S-Iceland
The Svalbard exemplar of Neoproterozoic Dr D Condon
glaciation
A study of clear sky closure study using high Dr J Pickering
resolution far-IR spectra from the high arctic
Seismic characterisation of subglacial Dr B Kulessa
conditions beneath the margin of the West
Greenland Ice Sheet
A new method for dating brittle Dr W Muller
deformation: U-Pb dating of carbonate fibres
Observations and synthesis to establish Dr D J Pearce
variability and trends of oceanic pH
Wave dynamics of the mesosphere Professor NJ Mitchell
Impact of copper geochemistry on the Professor DW Graham
selection and abundance of methane-
oxidizing bacteria in Arctic soils
MashMyData: Visualization and Dr JD Blower
intercomparison of environmental data on
the web
Flow dynamics and sedimentation in an Dr J Peakall
active submarine channel: a process-product
approach
Models and Impact Relevant climate Dr BN Lawrence
Prediction (MIRP)
A Novel Temperature and Salinity Dataset Dr SA Josey
for Northern High LAtitude Seas (ATLAS)
Development of a laser-based sea-ice Professor AS Brierley
chlorophyll sensor
Quantifying Event-Driven Methane Fluxes Dr Y Teh
from Northern Peatlands Using A Novel
Automated Flux Chamber Technique
The response of the Arctic regions to Dr RLH Essery
changing climate
Holocene Land-Ocean-Atmosphere Dr D Mauquoy
Interactions on the Eastern Seaboard of
North America
Holocene Land-Ocean-Atmosphere Professor F Street-Perrott
Interactions on the Eastern Seaboard of
North America
Holocene Land-Ocean-Atmosphere Dr P Hughes
Interactions on the Eastern Seaboard of
North America
Wave dynamics of the mesosphere Dr RE Hibbins
The response of the Arctic regions to Dr C Huntingford
changing climate
Are tropical uplands regional hotspots for Professor P Smith
methane and nitrous oxide?
The Svalbard exemplar of Neoproterozoic Dr IJ Parkinson
glaciation
The Svalbard exemplar of Neoproterozoic Professor IJ Fairchild
glaciation
Calibration and Cleaning of Magnetic Dr AW Thomson
Satellite Data
SEEBECK - using the Seebeck effect to power Mr M Rose
sea-ice instrumentation
Calibration and Cleaning of Magnetic Dr R Holme
Satellite Data
Understanding marine ice stream retreat Dr A Vieli
using numerical modelling and geophysical
data
Long-range atmospheric Nitrogen deposition Dr S McGowan
as a driver of ecological change in Arctic
lakes
Instantaneous and inverse coupling between Professor DA Hodell
the South and North Atlantic during the last
glacial period
ICE: Inuit Climate Experiment Dr JP Wilkinson
Early Concept for New Mission: A Dr M Macdonald
Spaceborne Multispectral Canopy Lidar
Early Concept for New Mission: A Dr I Woodhouse
Spaceborne Multispectral Canopy Lidar
SWARM data calibration and validation Professor MW Dunlop
Southern High Latitude Vegetation Response Dr U Salzmann
to Rapid Climate Change at the Cenozoic
Greenhouse to Icehouse Transition
Teeth and jaws: evolutionary emergence of a Dr M Purnell
model organogenic system and the adaptive
radiation of gnathostomes
SEEBECK - using the Seebeck effect to power Mr D Meldrum
sea-ice instrumentation
Combined genetic, morphological and Dr WEN Austin
ecological approaches to reduce uncertainty
in palaeoclimate reconstructions using
benthic foraminifers
Combined genetic, morphological and Dr K Darling
ecological approaches to reduce uncertainty
in palaeoclimate reconstructions using
benthic foraminifers
FEC for sailing participant on IODP Leg 318 Dr T Van De Flierdt
(Wilkes Land glacial history)
Long-range atmospheric Nitrogen deposition Dr J Kaiser
as a driver of ecological change in Arctic
lakes
Long-range atmospheric Nitrogen deposition Dr VJ Jones
as a driver of ecological change in Arctic
lakes
Long-range atmospheric Nitrogen deposition Professor NJ Anderson
as a driver of ecological change in Arctic
lakes
Investigating how environmental change Dr DJ Mayor
affects benthic biogeochemistry
Airborne Low Frequency Ice Sounder Mr H Corr
(ALFRIS)
RAPID-RAPIT Dr TJ Woollings
Understanding marine ice stream retreat Dr C Hillenbrand
using numerical modelling and geophysical
data
Teeth and jaws: evolutionary emergence of a Dr PCJ Donoghue
model organogenic system and the adaptive
radiation of gnathostomes
Synchronising marine and ice-core records Dr NJG Pearce
using tephrochronology (SMART)
RAPID-RAPIT Professor M Goldstein
MPhil in GIS and Remote Sensing. Masters Dr C Oppenheimer
Training Grant (MTG) to provide funding for
3 full studentships for two years
MRes Physics of the Earth and Atmosphere. Dr IM Brooks
Masters Training Grant (MTG) to provide
funding for 5 full studentships for two years.
Synchronising marine and ice-core records Dr WEN Austin
using tephrochronology (SMART)
Investigating the Dynamic Response of the Dr B Kulessa
Greenland Ice Sheet to Climate Forcing using
a Geophysical, Remote-Sensing and
Numerical Modelling Framework
Investigating the Dynamic Response of the Dr P Christoffersen
Greenland Ice Sheet to Climate Forcing using
a Geophysical, Remote-Sensing and
Numerical Modelling Framework
The NERC Earth System Science Graduate Dr A Jackson
School
The Eocene-Oligocene biotic turnover in the Dr MA Kaminski
North Atlantic and associated palaeoclimatic
change
Assessment of Cadmium Isotopes as a Dr M Rehkamper
Paleoclimate Proxy
Extending the timescales of glacier volume Professor T Murray
change in regions of GRACE-gravity
anomalies in Northern Greenland
Change in the Atlantic Atmosphere Ocean Dr MR Allen
System: ChAAOS
A holistic model of outlet calving, dynamic Dr A Hubbard
acceleration and drawdown for the
Greenland Ice Sheet
Instantaneous and inverse coupling between Dr S Barker
the South and North Atlantic during the last
glacial period
Synchronising marine and ice-core records Dr SM Davies
using tephrochronology (SMART)
RAPID-RAPIT Mr P Challenor
Improved models of West Antarctic glacial Dr MA King
isostatic adjustment through new crustal
motion data
Copepod sex ratio dynamics: the role of Dr AG Hirst
predators and food
RAPID-RAPIT Dr HL Johnson
Investigating the Dynamic Response of the Dr A Hubbard
Greenland Ice Sheet to Climate Forcing using
a Geophysical, Remote-Sensing and
Numerical Modelling Framework
Copepod sex ratio dynamics: the role of Dr CH Lucas
predators and food
Greening of retreating glaciers: storage Dr AJ Hodson
versus export of autochthonous organic
matter
Calibrating the fractionation of stable oxygen Dr J Tyler
and silicon isotopes in diatom silica through
laboratory culture experiments
A Laboratory Study of the Photolysis of the Dr CJ Percival
ClO Dimer
Greening of retreating glaciers: storage Dr AM Anesio
versus export of autochthonous organic
matter
Evolution of seawater Mg/Ca ratios since the Dr A Tripati
Cretaceous: New constraints from the
carbonate 'clumped isotope' thermometer.
High-resolution climate dynamics Dr M Joshi
A Laboratory Study of the Photolysis of the Dr W Bloss
ClO Dimer
Consistent multi-technique geodetic Professor PJ Clarke
estimates of present-day contributions to
regional sea level change
Application of elemental and isotopic ratios Professor DA Hodell
of bulk sediment and detrital carbonate to
identify and source Heinrich events in IODP
Exp 303/306 sites.
The role of atmospheric forcing on the Dr D Mair
dynamic stability of Greenland's outlet
glaciers
Proteomics: A novel approach to the study Dr E Dudley
of prey recognition by planktonic protists.
Constraints from new geochemical proxies Dr A Tripati
on temperature and sea level during critical
climate transitions.
The role of atmospheric forcing on the Dr PW Nienow
dynamic stability of Greenland's outlet
glaciers
The optical properties of black carbon Dr RG Grainger
The role of sea ice dynamics in carbonate Dr HA Kennedy
mineral production and its fate in the Polar
Oceans
Novel Ice Characterisation Experiment - Dr JK Jackson
Phase 1 (NICE-1)
Photochemical oxidation in snow and sea-ice Dr M King
by organic matter photocatalysis in the
visible: An international field and modelling
study.
The consequences of seasonal interactions in Dr S Bearhop
migratory birds: from individuals to
populations.
Isotopic constraints on the Arctic methane Professor EG Nisbet
budget
The genetic basis of maternal behaviour and Dr R Hager
parent-offspring conflict resolution in mice
Adjoint sensitivity of sea-level and inter- Professor DP Marshall
basin transports to surface forcing and
circulation anomalies in present and future
climates
A Century-long Record of Trace Gases in the Professor WT Sturges
Northern Hemisphere from the NEEM Ice
Core Drilling Project in Greenland
Quantifying the impact of anthropogenic and Professor K Carslaw
natural aerosol on Arctic climate
Estimating and reducing the uncertainty in Professor J Bamber
the future behaviour of the Greenland Ice
Sheet
Variability of the Denmark Strait Overflow Professor KJ Heywood
Modelling of Summertime Arctic Stratus Dr IM Brooks
Multiscale Analysis of Integrated and Species- Professor SC Olhede
Specific Response to Climate Forcing and
Eutrophication in Northern European Seas
Incorporation of frazil ice into a sea ice- Dr DL Feltham
ocean model
Shipboard studies of the influence of Professor EP Achterberg
inorganic seawater chemistry on calcareous
microplankton and the biological carbon
pump
Survival through the Arctic winter: How Dr K Wilson
gastrointestinal nematodes influence fitness
in reindeer.
Predicting Terrestrial CDOM Fate and Impact Dr V Le Fouest
on Plankton Productivity in the Rapidly
Changing Arctic Ocean
Partitioning of C, N and P between Professor KJ Flynn
particulate and dissolved phases during
growth of phytoplankton at different pH.
Towards improved estimation of carbon Dr R Baxter
balance in a low-Arctic mire: a
micrometeorological eddy covariance
approach to methane flux characterization.
Lability of organic carbon stored in Dr S Sjogersten
permafrost peatlands
Challenging the paradigm for plant-microbial Professor D Jones
resource partitioning in Antarctic
ecosystems
Thermal tolerances of Arctic and temperate Professor LS Peck
marine ectotherms under varying rates of
change
Impact of Arctic sea-ice retreat on Professor AS Brierley
zooplankton foraging behaviour and vertical
carbon flux
Present and Future Stability of Larsen C Ice Dr B Kulessa
Shelf (SOLIS)
Representing cloud inhomogeneity and Dr RJ Hogan
overlap in a General Circulation Model
Ikaite: A palaeoenvironmental proxy Dr REM Rickaby
Dynamics of gas hydrates in polar marine Professor T Minshull
environments.
Temporal evolution of the deep-sea Professor H Elderfield
carbonate system and implications for the
role of the oceans in glacial-interglacial
changes in atmospheric CO2
Ikaite: A palaeoenvironmental proxy Dr REM Rickaby
Modelling of the Wyville Thomson Ridge Dr V Vlasenko
overflow
Ikaite: A palaeoenvironmental proxy Dr REM Rickaby
Modelling of the Wyville Thomson Ridge Professor PA Davies
overflow
Ikaite: A palaeoenvironmental proxy Dr REM Rickaby
Investigating basal conditions and flow Dr P Christoffersen
dynamics on Vestfonna Ice Cap, Svalbard
Measuring and modelling the Raymond Dr RCA Hindmarsh
Effect for to infer low strain-rate ice
rheology
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
Biohopanoid markers as tracers of methane Professor T Wagner
emission and oxidation events in the
Quaternary ocean
High spatio-temporal resolution changes in Dr MA King
Earth's gravity field from GOCE with
application to ice mass balance
Continental and oceanic upper mantle Dr S Rost
structure from seismic array data
Dynamics of gas hydrates in polar marine Professor C Berndt
environments.
Rapid evolution of phenotypic divergence in Professor IA Johnston
fish populations
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
FAGE measurements of OH, HO2 and IO Professor D Heard
during COBRA
Arctic Sea Ice Dynamics Using Experiments Dr DL Feltham
and Multi-scale Modelling
Biogenic production of climatic amplifiers Dr JL wadham
under ice
Understanding the role and significance of Dr CJ Halsall
the Arctic for the cycling and fate of
persistent organic pollutants (ARCPOP)
Turbulent Exchange in the Arctic Boundary Dr IM Brooks
Layer
New particles in the atmosphere: two non- Professor JMC Plane
classical examples
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
Marine geophysical and geological Professor C O'Cofaigh
investigations of past flow and stability of a
major Greenland ice stream in the Late
Quaternary
Convection and Cascading on Arctic Shelves: Dr FR Cottier
a tracer study
Rapid deployment of a seismic network to Professor A Rietbrock
record the aftershocks of the Mw=6.2 Aisen
earthquake in Southern Chile
GOING UNDERGROUND: HUMAN Professor S Banwart
PATHOGENS IN THE SOIL-WATER
ENVIRONMENT
Ocean teleconnections between Antarctica Dr NC Wells
and the Equatorial Pacific and Atlantic.
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
Arctic Synoptic Basin-wide Oceanography. Dr SW Laxon
Impact of combined iodine and bromine Professor LJ Carpenter
release on the Arctic atmosphere (COBRA).
Windows into the Deep: An Investigation of Professor M Walter
Ultradeep Mineral Inclusions in Natural
Diamonds
GOING UNDERGROUND: HUMAN Professor S Banwart
PATHOGENS IN THE SOIL-WATER
ENVIRONMENT
Predator-prey interactions and the evolution Professor J Krause
of prey aggregation
Impact of combined iodine and bromine Professor LJ Carpenter
release on the Arctic atmosphere (COBRA).
Impact of combined iodine and bromine Professor LJ Carpenter
release on the Arctic atmosphere (COBRA).
Impact of combined iodine and bromine Professor LJ Carpenter
release on the Arctic atmosphere (COBRA).
Climate change in the Holocene: A multi- Professor S Belt
proxy case study
Hudson Bay Lithospheric Experiment Professor M Kendall
Southern Hemisphere climate change in an Professor IA Renfrew
era of ozone recovery
New particles in the atmosphere: two non- Professor JMC Plane
classical examples
Marine geophysical and geological Professor C O'Cofaigh
investigations of past flow and stability of a
major Greenland ice stream in the Late
Quaternary
Quantifying Flood Risk of Extreme Events Dr PE McSharry
using Density Forecasts Based on a New
Digital Archive and Weather Ensemble
Predictions
Dynamics of gas hydrates in polar marine Professor C Berndt
environments.
Numerical testing of hypotheses for the Dr A Vieli
recent thinning and acceleration of
Greenland outlet glaciers
Testing the instability theory of subglacial Professor CD Clark
bedform production
A novel proxy for Arctic sea-ice Professor S Belt
Global data synthesis of air-sea fluxes of Professor PS Liss
gases and aerosols for policy-directed
modelling and assessment of climate change
and pollution
Arctic Biosphere-Atmosphere Coupling Dr M Williams
across multiple Scales (ABACUS).
Assimilation in ocean and coupled models to Professor K Haines
determine the thermohaline circulation.
Testing the instability theory of subglacial Professor CD Clark
bedform production
MRes Physics of the Earth and Atmosphere Dr IM Brooks
Master of Philosophy in GIS and Remote Dr C Oppenheimer
Sensing
Can radiocarbon dating chironomid head Dr P Langdon
capsules increase chronological accuracy in
lake sediments?
Greenland Flow Distortion. Professor IA Renfrew
Is increased chemical complexity of Professor G Underwood
extracellular polymeric substances (EPS)
related to increasing salinity in polar sea ice?
Arctic Biosphere-Atmosphere Coupling Dr M Williams
across multiple Scales (ABACUS).
Physics and Chemistry of Frost-Flowers and Professor MH Smith
Their Resultant Sea -Salt Aerosol
Assessing the role of ocean circulation in Professor H Elderfield
rapid climate change through the novel
integration of high-resolution proxy records
Arctic Biosphere-Atmosphere Coupling Dr M Williams
across multiple Scales (ABACUS).
Arctic Biosphere-Atmosphere Coupling Dr M Williams
across multiple Scales (ABACUS).
Pioneering post-genomics approaches for Dr FC Kuepper
studying algal host-pathogen interactions,
using the ectocarpus/eurychasma model.
Using records of large mammal populations Dr B Shapiro
in the Urals to decipher the timing and
effects of global climate change.
Arctic Biosphere-Atmosphere Coupling Dr M Williams
across multiple Scales (ABACUS).
Physics and Chemistry of Frost-Flowers and Dr A Jackson
Their Resultant Sea -Salt Aerosol
Tropical Biomes in Transition Dr S Sitch
Paleogene orbitally calibrated climate cycles Dr H Palike
A time series of magma flux measurements Professor G Wadge
at the lava dome of Soufriere Hills Volcano,
Montserrat
Constraining Greenland ice sheet mass Dr G Milne
balance using proxy sea-level records.
Microbial community metabolism and Dr AM Anesio
carbon budget on glaciers
Constructing a tephrochronology framework Dr SM Davies
for the last interglacial - glacial transition
Global change in the Stratosphere and its Dr A Charlton-Perez
impact on Tropospheric Climate
Genetic bottlenecks and the geographic Professor D Charlesworth
distribution of sexual and asexual organisms
Collaborative Autosub Science in Extreme Professor G Griffiths
Environments
Global Modelling of Aerosols and Chemistry Professor K Carslaw
in Support of SOLAS-UK
Low temperature reactivity of tropospheric Dr RA Cox
aerosols
The genetics of mammalian speciation and Dr I Barnes
extinction in the Late Pleistocene
Reducing the Impact of Orbit Error on the Professor M Ziebart
Measurement of Polar Ice Thickness and Sea
Level Variations.
NDG2: The NERC DataGrid and associated Dr BN Lawrence
toolkit.
Taxonomic marine plankton identification Professor G Pierce
manual for North European seas.
Cirrus and Anvils European Satellite and Dr R Siddans
Airborne Radiation measurements project.
Cirrus and Anvils European Satellite and Dr R Siddans
Airborne Radiation measurements project.
NDG2: The NERC DataGrid and associated Dr BN Lawrence
toolkit.
Biomass mapping upon Arctic glaciers using Dr AJ Hodson
high resolution aerial survey of cryoconite
holes.
Biostratigraphy and Paleoceanographic Dr MA Kaminski
significance of Benthic Foraminifera from the
Lomonosov Ridge.
Changes in glacier geometry and extent in Professor T Murray
Svalbard: Implications for sea-level rise
during the 20th and 21st centuries.
Greenland Flow Distortion. Professor IA Renfrew
A new geochemical proxy for past climates Dr G Masse
Arctic regulation of the thermohaline Dr S Bacon
circulation (ARTHER)
NDG2: The NERC DataGrid and associated Dr BN Lawrence
toolkit.
NDG2: The NERC DataGrid and associated Dr BN Lawrence
toolkit.
Assimilation in ocean and coupled models to Professor K Haines
determine the thermohaline circulation.
Arctic regulation of the thermohaline Dr S Bacon
circulation (ARTHER)
A matter of taste: revealing underlying Dr E Roberts
mechanisms behind recognition of prey by
protozooplankton, focusing on the role of
the Mannose-Binding Lectin.
The North Atlantic Ice-Climate System: Dr WEN Austin
Reconstructing the Provenance and Phasing
of Ice Rafting Events using Palaeointensity
Assisted Chronologies.
Do herbivores decrease tundra carbon sink Dr SJ Woodin
strength by reducing the moss layer?
A seasonally resolved record of the 13C Dr WEN Austin
Suess Effect in the NE Atlantic, 1948-present
Effect of the spatial variability of physical Dr BP Hubbard
parameters on the rheology of temperate
glaciers and their modelled response to
climate change.
Acoustic Navigation System. Mr DM Blake
Arctic regulation of the thermohaline Dr S Bacon
circulation (ARTHER)
Advanced Global Barotropic Ocean Professor CW Hughes
Modelling for Application to Studies of
Climate Change and Ocean Dynamics.
BDAN: Big Data Analysis Network. Dr BN Lawrence
Deep ocean convection: observations from Dr DA Smeed
an adaptive network of underwater gliders.
Slope stability on Europe's passive Professor JA Dowdeswell
continental margins.
Using benthic foraminiferal Mg/Ca at ODP Professor H Elderfield
site 982 to assess the climatic response to
orbital and greenhouse gas forcing during
the late Pleistocene.
Plant responses to abiotic stress at range Professor WE Kunin
margins: mechanisms and limits to
adaptation.
Plant responses to abiotic stress at range Professor WE Kunin
margins: mechanisms and limits to
adaptation.
Determining microzooplankton parameters Dr D Montagnes
for spatial and seasonal modelling of the
Irminger Basin.
Time series of Transient Tracers in the North Professor A Watson
Atlantic.
Atmospheric teleconnections with the Professor LJ Gray
tropical stratosphere.
A physiochemically-stable seawater culturing Dr WEN Austin
system to constrain elemental and isotopic
proxies in benthic foraminiferal calcite.
Bottom Turbulence Kit. Professor J Huthnance
Changes in glacier geometry and extent in Professor T Murray
Svalbard: Implications for sea-level rise
during the 20th and 21st centuries.
Mass spectrometer & sampling systems for Professor H Elderfield
isotopic analysis of oxygen, carbon,
hydrogen & deuterium for the
environmental sciences.
What are the roles of DMS and other simple Dr M Steinke
molecules as signalling compounds in marine
tritrophic interactions?
5 Oceanographic pCO2 Systems for NERC Dr NJ Hardman-Mountford
research fleet. 1 CARIOCA buoy.
Changes in glacier geometry and extent in Professor T Murray
Svalbard: Implications for sea-level rise
during the 20th and 21st centuries.
A statistical approach for estimating the Professor AJ Payne
contribution of glaciers to future sea-level
rise.
Probing the early history of the Earth from Dr FM Stuart
the volatile inventory of the deep mantle.
Quantifying the effect of weathering Professor KW Burton
processes on the chemical signal to the
oceans.
Stadial - Interstadial changes in deep-water Professor H Elderfield
circulation and sources in the Northeast
Atlantic and their association with rapid sea
level rise.
Laboratory simulation of solifluction Professor C Harris
processes associated with one-sided and two-
sided active-layer freezing.
UK-HIGEM: a national programme in 'Grand Professor JM Slingo
Challenge' high resolution modelling of the
global environment.
Size structures of Calanus finmarchicus Professor CJ Secombes
populations and of planktonic predators in
the Irminger Basin.
Does resource partitioning maintain plant Professor R Bardgett
species diversity in nitrogen limited
ecosystems?
A trans-Atlantic comparison of the relative Professor AS Brierley
overwintering depths of Calanus and its
predators: setting the Irminger Sea in a
wider geographic context.
Effect of the spatial variability of physical Dr BP Hubbard
parameters on the rheology of temperate
glaciers and their modelled response to
climate change.
Effect of the spatial variability of physical Dr BP Hubbard
parameters on the rheology of temperate
glaciers and their modelled response to
climate change.
Identification and characterisation of ice Dr CR Stokes
stream sticky spots: an improved
understanding of ice stream basal mechanics
and shutdown.
Investigating genetic records preserved in Dr B Shapiro
sedimentary deposits: The effects of
environmental change on plant diversity and
composition.
Effect of the spatial variability of physical Dr BP Hubbard
parameters on the rheology of temperate
glaciers and their modelled response to
climate change.
Laboratory studies of key reactions of CIO Dr D Rowley
affecting atmospheric ozone abundances.
UK-HIGEM: a national programme in 'Grand Professor JM Slingo
Challenge' high resolution modelling of the
global environment.
Carbon fluxes in grassland soils: the control Professor J Farrar
and predictive value of soil respiration.
Better understanding of Open Ocean Deep Professor CC Pain
Convection (OODC) with reference to THC.
UK-HIGEM: a national programme in 'Grand Professor JM Slingo
Challenge' high resolution modelling of the
global environment.
Cape Farewell and Eirik Ridge: interannual to Dr S Bacon
millennial Thermohaline Circulation
variability.
Evolutionary lessons from the extinct giant Dr B Shapiro
American cats: phylogeography,
palaeoecology, and extinction of
sabertooths, cheetahs and lions.
A detailed study of two Pleistocene magnetic Dr C MacNiocaill
excursions: their duration, spatial variability
and their effect on cosmogenic nuclide
production.
Processes controlling dense water formation Professor AJ Willmott
and transport on Arctic shelves.
Processes controlling dense water formation Professor AJ Willmott
and transport on Arctic continental shelves.
The role of salinity in ocean circulation and Dr E Guilyardi
climate response to greenhouse gas forcing.
Cell-surface mechanisms for the recognition Dr E Roberts
of prey by marine bacterivorous
protozooplankton.
Proposal for an Isaac Newton Institute (INI) Professor JMNT Gray
satellite meeting on Geophysical Granular
and Particle-Laden Flows.
UK-HIGEM: a national programme in 'Grand Professor JM Slingo
Challenge' high resolution modelling of the
global environment.
ISOTOPE: Ice Shelf Oceanography: Professor KJ Heywood
Transports, Oxygen-18 and Physical
Exchanges.
The role of the cryosphere in modulating the Professor J Bamber
thermohaline circulation of the North
Atlantic.
The vortex dynamics of the polar vortex- Professor DG Dritschel
Aleutian high system: a systematic study of
stability and non-linear interaction.
The role of sea ice on seasonal to decadal Professor PJ Valdes
variability in the North Atlantic.
Circulation, overflows and convection in the Professor A Watson
Nordic Seas studied using tracers and
models.
High resolution anatomy of rapid climate Dr EW Wolff
transitions from a Greenland ice core.
In situ measurement of profiles of brine Professor MG Worster
volume in growing sea ice.
In search of the earliest seed plants. Professor JEA Marshall
Time series of transient tracers in North Professor A Watson
Atlantic deep waters.
New acoustic technology for zooplankton Professor AS Brierley
sampling: Total Target Strength of
Meganyctiphanes norvegica, and variation of
TTS with size and maturity.
ISOMAP-UK: a combined data-modelling Professor JA Holmes
investigation of water isotopes and their
interpretation during rapid climate-change
events.
Crustal melting and lithosphere strength in Professor J Grocott
collisional orogens: an evaluation of channel
flow.
Marine geological processes and sediments Professor JA Dowdeswell
beneath floating ice shelves in Greenland
and Antarctica: investigations using the
Autosub AUV.
A field and modelling study of snowpack Dr M King
photochemistry in mid-latitude (British)
snowpacks.
Laboratory studies of the dynamics of Professor JP Reid
aerosol droplets.
Global marine sources of reactive halogen Professor LJ Carpenter
species.
Using late Pleistocene DNA to examine the Dr B Shapiro
effects of paleoenvironmental change.
Climate, snow and hydrology in tundra Dr R Baxter
ecosystems interactions, feedbacks and
scaling issues.
Climate, snow and hydrology in tundra Dr R Baxter
ecosystems interactions, feedbacks and
scaling issues.
Scaling of snow processes over complex Dr RLH Essery
landscapes for atmospheric and hydrological
modelling applications.
The NERC Datagrid. Dr BN Lawrence
GODIVA: Grid for Ocean Diagnostics, Professor K Haines
Interactive Visualisation and Analysis.
Measuring snow accumulation in the Mr J Cooper
Canadian High Arctic using an ice geophysical
logging system.
The role of sea ice on seasonal to decadal Professor PJ Valdes
variability in the North Atlantic.
Molecular and morphological phylogeny of Dr PJ Hayward
the cheilstomate Bryzoa.
Agulhas 'Leakage' and abrupt climate Professor R Zahn
change: the past 50,000 years.
GODIVA: Grid for Ocean Diagnostics, Professor K Haines
Interactive Visualisation and Analysis.
GODIVA: Grid for Ocean Diagnostics, Professor K Haines
Interactive Visualisation and Analysis.
Observation and modelling of coastal Professor P Wadhams
polynyas and sea ice processes in the
Antarctic and Arctic.
Photoelectric emission from mesospheric ice Professor JMC Plane
particles.
Trophic interactions of copepods - Professor KJ Flynn
application of natural abundance of stable
isotopes.
GODIVA: Grid for Ocean Diagnostics, Professor K Haines
Interactive Visualisation and Analysis.
Interannual variability associated with the Professor LJ Gray
QBO and its impact on the UTLS region.
The controls on marine benthic biodiversity Professor P Tyler
and standing stock in ice covered
environments.
GODIVA: Grid for Ocean Diagnostics, Professor K Haines
Interactive Visualisation and Analysis.
Bedrock fracture by ice segregation. Dr J Murton
Diversity and biogeography of Antarctic deep- Professor AJ Gooday
sea foraminiferal species: molecular vs
morphological approaches.
Retrieval of polar stratospheric cloud Professor K Carslaw
microphysical properties from multi-
wavelength satellite extinction and lidar
measurements.
Latitudinal temperature gradients and the Dr NM Whiteley
evolutionary adaptation of heavy chain
myosin genes in gammarid amphipods.
On the evolution of observed oceanic heat Professor K Haines
anomalies and those in HADCM3.
Impact of iodine compounds on the coupling Professor RP Wayne
of NOx and HOx chemistry in the marine
boundary layer, the troposphere, and the
lower stratosphere.
Dev & app of comb UV Photoelec Professor J Dyke
Spectrometer/Photoionisation mass spectro
coupled with disch-flow sys for study of gas-
phase kinetics of red S species
The nature and origin of cryptic species of Professor M Kucera
modern planktonic foraminifera: developing
a new proxy for palaeoclimate, evolution
and biodiversity.
Dev & app of comb UV Photoelec Professor J Dyke
Spectrometer/Photoionisation mass spectro
coupled with disch-flow sys for study of gas-
phase kinetics of red S species
Optimisation of an Arctic sea ice model using Dr SW Laxon
spaceborne estimates of ice thickness.
Hydrothermal activity along the Knipovich Professor CR German
Ridge: 74-78 degrees N , Norwegian-
Greenland Sea.
Pine Island Glacier flow and dynamics. Professor AJ Payne
Genetic variation in Antarctic lichens. Dr PD Crittenden
Mass balance of Svalbard glaciers and ice Professor J Bamber
caps using high-accuracy airborne laser
altimetry.
Investigation of ozone loss and dynamic Professor JA Pyle
processes in the lower stratosphere using
models and atmospheric tracer
measurements.
Environmental and genetic mechanisms Professor IA Johnston
underlying different muscle growth patterns
in Arctic charr (Salvelinus alpinus) morphs.
Limb-sounding of stratos BrO & CIO by a high- Professor B Ellison
sensitivity (SIS) balloon-borne 500 GHz
receiver in prep for an ESA Atmospheric
Chem explorer mission
Benthic foraminifera from northern Dr MA Kaminski
Norwegian Sea: their biostratigraphy and
paleoceanographical significance.
Modelling DON dynamics in arctic tundra Professor D Jones
and temperate grassland ecosystems.
Palaeolimnological evidence for circumarctic Dr VJ Jones
climate warming in Northern Russia
Millennial-scale oceanic variability during the Dr MR Chapman
penultimate glacial-interglacial climate cycle.
Ichthyostega revealed: anatomy, Professor JA Clack
systematics, phylogeny, sedimentary and
faunal contexts, and its true place in
tetrapod origins.
A novel instrument for IO and NO2 detection Professor A J Orr-Ewing
based on cavity ring-down spectroscopy.
Architectural analysis of glacier-influenced Professor JA Dowdeswell
margin sediments using seismic records from
the Late Ordovician of Northern Africa.
Salinity minima in the Nordic and Arctic Seas: Professor GR Bigg
coupled climate anomalies?
Winter Coccolithophores in the Bering Sea? Dr T Tyrrell
Ichthyostega revealed: anatomy, Professor JA Clack
systematics, phylogeny, sedimentary and
faunal contexts, and its true place in
tetrapod origins.
Modelling nitrogen fluxes in tundra ecosys Professor J Laybourn-Parry
on Svalbard (78o N)using 15 N-labelling of
snowpack & measure of natural isotopic
abund 18 O/16 O & 15N/14N
Latitudinal clines in physiological capacities Professor LS Peck
and upper limits in Antarctic marine
invertebrates.
Representation of snow ablation processes Professor JW Pomeroy
for land surface schemes
Palaeobiology of the white sea Ediacaran Dr NJ Butterfield
Biota, NW Russia
Quantitative calibration of lake sediments as Professor R Thompson
climatic recorders of ice-cover duration
Modelling wind and buoyancy driven flow in Professor AJ Willmott
the mid-latitude and polar oceans.
Data assimilation of aerosol and chemical Dr D Lary
constituents.
Quantifying role of snow in delivering Professor K Jones
persistent organic pollutants (POPS) to a
northern catchment & understanding their
behaviour in the snow pack
Field and isotopic investigations of early Dr CRL Friend
Archaean rocks in west Greenland and their
bearing on early crustal genesis and the
evolution of continenta
Photochemical NOX production in polar Dr EW Wolff
snow - controlling factors and quantification
Development of a global model growth and Dr AG Hirst
fecundity in marine planktonic copepods:
accounting for food availability.
Modelling the persistence of zooplankton in Dr GA Tarling
the Irish Sea using optimal vertical migration
patterns.
Kinetics and minor channel branching in key Dr D Rowley
atmospheric halogen reactions
Direct and plant-mediated responses of Dr CH Robinson
biodiversity and ecosystem function of
decomposer fungi to nitrogen enrichment in
a High Arctic ecosystem
Scaled centrifuge modelling of periglacial Professor C Harris
mass movement processes
Non-methane hydrocarbons and dimethyl Professor AC Lewis
sulphide in the Arctic troposphere.
Controls upon the magnitude, timing and Dr AJ Hodson
bioavailability of terrestrial nutrient delivery
to high Arctic fjords
Signals for nitrogen deposition load in mat- Dr PD Crittenden
forming lichens
Stability of the Antarctic ice sheet: a Professor AJ Payne
numerical analysis
Forecast and analysis of polar stratospheric Professor K Carslaw
clouds and cirrus for the NASA-SOLVE Arctic
ozone campaign
Multi-annual dynamics and mass balance of Professor T Murray
Svalbard glaciers
Procurement, installation and support for a Professor JA Dowdeswell
multibeam echo sounder on rss james clark
ross, the ice-strengthened scientific research
vessel
Temperature effects on the partitioning Professor H Jones
between respiratory pathways in plants
Ice dynamics and runoff in High Arctic Dr PW Nienow
glaciers and response to climate change
Laboratory, theoretical and modelling Dr D Rowley
studies of gas phase peroxy radical reactions
affecting the UTLS HOx budget
Geometry and Dynamics of Large Ice Caps in Professor JA Dowdeswell
the Canadian High Arctic
Ice dynamics and mass flux of Arctic Ice Caps Professor DJ Wingham
and the Greenland Ice Sheet using satellite
radar interferometry
Polar microbial survival strategies Professor J Laybourn-Parry
Novel approach to the determination of the Dr G Nickless
very volatile fluorinated compounds by
automated gas chromatography-mass
spectrometry
The global methane budget: constraints Professor EG Nisbet
from the Atlantic sector
An investigation of the dynamics driving the Professor P Sammonds
responses of ice caps to climatic forcing
Measuring and modelling surface fluxes in Professor S Mobbs
the marginal ice zone
Late Quaternary ice sheet dynamics in West Professor A Long
Greenland
Three-dimensional model studies for Professor M Chipperfield
THESEO
Using permafrost dna to analyse the ice age Professor A Cooper
paleoecology of large mammals
Inter-hemispheric 14C offsets: temporal Dr FG McCormac
variations
A general circulation model study of Professor KP Shine
ozone/temperature interactions
Sea ice and oceanic vertical circulation Dr S Bacon
(arcice)
The influence of ice and fresh water on the Professor A Watson
Nordic Seas thermohaline circulation: a
study using SF6 and d18 0
Ancient DNA analysis of Beringian Professor A Cooper
palaeoecology in the Late Pleistocene
An investigation of the dynamics driving the Professor JK Hart
responses of ice caps to climatic forcing
Measuring and modelling surface fluxes in Dr MJ Yelland
the marginal ice zone
Measuring and modelling surface fluxes in Dr JC King
the marginal ice zone
Novel noble gas isotope ratio analyser: Mr PF Dennis
applications in hydrogeology, palaeoclimate
studies and oceanography
High resolution modelling of the Arctic sea Dr DJ Webb
ice and ocean circulation
Multi-annual dynamics and mass balance of Professor T Murray
Svalbard glaciers
Geophysical and geological investigations of Professor JA Dowdeswell
sedimentation and ice-ocean variability on
arctic continental margins. (arcice)
Sea ice and oceanic vertical circulation Professor P Wadhams
(arcice)
Understanding and improving the Professor PJ Valdes
representation of Arctic land ice in
atmospheric GCMs
Multi-annual dynamics and mass balance of Professor T Murray
Svalbard glaciers
Multi-annual dynamics and mass balance of Professor T Murray
Svalbard glaciers
The hydrochemistry of runoff from large Professor M Tranter
terrestrial ice masses on crystalline bedrock
Chemical weathering in the proglacial zone - Professor M Tranter
source or sink of CO2?
Arctic Ocean circulation and ice freeboard Dr SW Laxon
through space-borne altimetry
Advective ecology of zooplankton in the Dr GA Tarling
clyde sea area
High Resolution Dynamics Limb Sounder Dr JJ Barnett
(HIRDLS)
Mechanisms of formation and palaeo- Professor A Kemp
significance of Cretaceous diatomites
The use of cryomicroscopy to elucidate Dr J G Day
modes of freeze-induced injury in protists
Ocean freezing: marrying theoretical, Professor H Huppert
experimental and field studies
The role of halogens in stratospheric ozone Dr D Rowley
chemistry
High Resolution Dynamics Limb Sounder Dr JJ Barnett
(HIRDLS)
Atmospheric, oceanic and planetary physics Dr JJ Barnett
(hirdls)
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University of Southampton, School of Ocean University of Southampton, School of Ocean 1-Apr-11
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Scottish Association For Marine Science, Scottish Association For Marine Science, 1-Feb-11
Scottish Association For Marine Science Scottish Association For Marine Science
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University of Liverpool, Oceans and National Oceanography Centre, Science and 1-Feb-11
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Marine Biological Association, Marine Marine Biological Association, Marine 1-Feb-11
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University of Bath, Electronic & Electrical Eng University of Bath, Electronic & Electrical Eng 17-May-10
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University College London, Earth Sciences Scottish Association For Marine Science, 1-Jun-07
Scottish Association For Marine Science
University College London, Earth Sciences National Oceanography Centre, Science and 1-Jun-07
Technology
University College London, Earth Sciences University College London, Mullard Space 1-Jun-07
Science Laboratory
University of York, Chemistry The University of Manchester, Earth 10-Apr-07
Atmospheric and Env Sciences
University of Bristol, Earth Sciences University of Bristol, Earth Sciences 5-Apr-07
University of Sheffield, Civil and Structural University of Sheffield, Civil and Structural 1-Apr-07
Engineering Engineering
Humboldt University Berlin, Humboldt University of Leeds, Inst of Integrative & 1-Apr-07
University Berlin Comparative Biolog
University of York, Chemistry University of Leeds, Sch of Chemistry 1-Apr-07
University of York, Chemistry University of York, Chemistry 29-Mar-07
University of York, Chemistry NERC British Antarctic Survey, Physical 19-Mar-07
Sciences
University of Plymouth, Sch of Geog Earth & University of Plymouth, Sch of Earth Ocean 1-Mar-07
Environ Sciences and Environment
University of Bristol, Earth Sciences University of Bristol, Earth Sciences 1-Mar-07
University of East Anglia, Environmental University of East Anglia, Environmental 1-Mar-07
Sciences Sciences
University of Leeds, Sch of Chemistry University of Leeds, Sch of Chemistry 1-Feb-07
Durham University, Geography University of Cambridge, Scott Polar 1-Feb-07
Research Institute
University of Oxford, Smith School of University of Oxford, Engineering Science 1-Jan-07
Enterprise and the Env
Geomar Research Centre, UNLISTED Royal Holloway, Univ of London, Earth 1-Jan-07
Sciences
Durham University, Geography Durham University, Geography 1-Dec-06
University of Sheffield, Geography University of Oxford, Mathematical Institute 1-Dec-06
University of Plymouth, Sch of Geog Earth & University of Plymouth, Sch of Earth Ocean 28-Nov-06
Environ Sciences and Environment
University of East Anglia, Environmental University of East Anglia, Environmental 15-Nov-06
Sciences Sciences
University of Edinburgh, Sch of Geosciences University College London, Geography 1-Nov-06
University of Reading, Environmental University of Southampton, School of Ocean 1-Oct-06
Systems Science Centre and Earth Science
University of Sheffield, Geography University of Sheffield, Geography 14-Sep-06
University of Leeds, School of Earth and University of Leeds, School of Earth and 1-Sep-06
Environment Environment
University of Cambridge, Geography University of Cambridge, Geography 1-Sep-06
University of Southampton, School of University of Southampton, School of 1-Aug-06
Geography Geography
University of East Anglia, Environmental University of Reading, Meteorology 1-Aug-06
Sciences
University of Essex, Biological Sciences University of Essex, Biological Sciences 1-Jul-06
University of Edinburgh, Sch of Geosciences Durham University, Biological and 1-Jul-06
Biomedical Sciences
University of Leeds, School of Earth and NERC British Antarctic Survey, Physical 6-Jun-06
Environment Sciences
University of Cambridge, Earth Sciences University of Cambridge, Earth Sciences 5-Jun-06
University of Edinburgh, Sch of Geosciences University of Sheffield, Animal and Plant 1-Jun-06
Sciences
University of Edinburgh, Sch of Geosciences University of Stirling, Biological and 1-Jun-06
Environmental Sciences
Scottish Association For Marine Science, Scottish Association For Marine Science, 29-May-06
Scottish Association For Marine Science Scottish Association for Marine Science
Pennsylvania State University, Biology University of Oxford, Zoology 1-May-06
University of Edinburgh, Sch of Geosciences University of York, Biology 1-May-06
University of Leeds, School of Earth and University of Leeds, School of Earth and 1-May-06
Environment Environment
University of Leeds, Sch of Geography University of Sheffield, Animal and Plant 1-May-06
Sciences
University of Southampton, School of Ocean University of Southampton, School of Ocean 26-Apr-06
and Earth Science and Earth Science
University of Reading, Environmental University of St Andrews, Physics and 19-Apr-06
Systems Science Centre Astronomy
University of Ottawa, Earth Sciences Durham University, Earth Sciences 1-Apr-06
University of Bristol, Geographical Sciences Aberystwyth University, Inst of Biological, 10-Mar-06
Environ & Rural Sci
Swansea University, School of the Swansea University, Geography 27-Feb-06
Environment and Society
University of Reading, Meteorology University of Reading, Meteorology 6-Feb-06
University of Edinburgh, Inst of Evolutionary University of Edinburgh, Inst of Evolutionary 1-Feb-06
Biology Biology
National Oceanography Centre, Science and National Oceanography Centre, NERC 24-Jan-06
Technology Strategic Research Division
University of Leeds, School of Earth and University of Leeds, School of Earth and 3-Jan-06
Environment Environment
University of Cambridge, Chemistry University of Cambridge, Chemistry 1-Jan-06
Royal Holloway, Univ of London, Biological Royal Holloway, Univ of London, Biological 14-Nov-05
Sciences Sciences
University College London, Civil University College London, Civil 7-Nov-05
Environmental and Geomatic Eng Environmental and Geomatic Eng
STFC - Laboratories, Space Science & Plymouth Marine Laboratory, Plymouth 1-Nov-05
Technology (SSTD) Marine Lab
University of Aberdeen, Inst of Biological and University of Aberdeen, Inst of Biological and 24-Oct-05
Environmental Sci Environmental Sci
STFC - Laboratories, Space Science & Imperial College London, Dept of Physics 10-Oct-05
Technology (SSTD)
STFC - Laboratories, Space Science & STFC - Laboratories, Space Science & 10-Oct-05
Technology (SSTD) Technology (SSTD)
STFC - Laboratories, Space Science & Proudman Oceanographic Laboratory, 3-Oct-05
Technology (SSTD) Proudman Oceanographic Laboratory
University of Sheffield, Geography University of Sheffield, Geography 1-Oct-05
University College London, Earth Sciences University College London, Earth Sciences 1-Oct-05
Swansea University, School of the University of Bristol, Geographical Sciences 1-Oct-05
Environment and Society
University of East Anglia, Environmental University of East Anglia, Environmental 1-Oct-05
Sciences Sciences
University of Plymouth, Sch of Geog Earth & University of Plymouth, Sch of Earth Ocean 27-Sep-05
Environ Sciences and Environment
National Oceanography Centre, Science and University of East Anglia, Mathematics 26-Sep-05
Technology
STFC - Laboratories, Space Science & National Oceanography Centre, NERC 12-Sep-05
Technology (SSTD) Strategic Research Division
STFC - Laboratories, Space Science & STFC - Laboratories, Space Science & 1-Sep-05
Technology (SSTD) Technology (SSTD)
University of Reading, Environmental University of Reading, Environmental 1-Sep-05
Systems Science Centre Systems Science Centre
National Oceanography Centre, Science and University College London, Mullard Space 1-Aug-05
Technology Science Laboratory
Swansea University, School of the Swansea University, Biological Sciences 1-Jul-05
Environment and Society
University of St Andrews, Geography and University of St Andrews, Geography and 13-Jun-05
Geosciences Geosciences
University of Aberdeen, Inst of Biological and University of Aberdeen, Biological Sciences 1-Jun-05
Environmental Sci
University of St Andrews, Geography and University of St Andrews, Geography and 1-Jun-05
Geosciences Geosciences
Aberystwyth University, Inst of Geography Swansea University, Geography 1-May-05
and Earth Sciences
NERC British Antarctic Survey, Corporate NERC British Antarctic Survey, UNLISTED 30-Apr-05
Services
National Oceanography Centre, Science and National Oceanography Centre, NERC 12-Apr-05
Technology Strategic Research Division
National Oceanography Centre, Science and Proudman Oceanographic Laboratory, 1-Apr-05
Technology Proudman Oceanographic Laboratory
STFC - Laboratories, Space Science & STFC - Laboratories, Space Science & 10-Mar-05
Technology (SSTD) Technology (SSTD)
National Oceanography Centre, Science and National Oceanography Centre, NERC 9-Feb-05
Technology Strategic Research Division
University of Cambridge, Scott Polar University of Cambridge, Scott Polar 4-Feb-05
Research Institute Research Institute
University of Cambridge, Earth Sciences University of Cambridge, Earth Sciences 1-Feb-05
University of Leeds, Inst of Integrative & University of Leeds, Inst of Integrative & 1-Feb-05
Comparative Biolog Comparative Biolog
University of Leeds, Inst of Integrative & University of Sheffield, Animal and Plant 1-Feb-05
Comparative Biolog Sciences
University of Liverpool, Sch of Biological University of Liverpool, Sch of Biological 15-Jan-05
Sciences Sciences
University of East Anglia, Environmental University of East Anglia, Environmental 4-Jan-05
Sciences Sciences
University of Oxford, Oxford Physics University of Reading, Meteorology 1-Jan-05
University of St Andrews, Geography and University of St Andrews, Geography and 1-Jan-05
Geosciences Geosciences
National Oceanography Centre, Science and Proudman Oceanographic Laboratory, 8-Dec-04
Technology Proudman Oceanographic Laboratory
Swansea University, School of the Newcastle University, Civil Engineering and 1-Nov-04
Environment and Society Geosciences
University of Cambridge, Earth Sciences University of Cambridge, Earth Sciences 1-Oct-04
University of Essex, Biological Sciences University of East Anglia, Environmental 1-Oct-04
Sciences
Plymouth Marine Laboratory, CASIX Plymouth Marine Laboratory, Plymouth 1-Oct-04
Marine Lab
Swansea University, School of the Swansea University, Geography 1-Oct-04
Environment and Society
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 1-Sep-04
Scottish Universities Env Research Cen, Scottish Universities Env Research Cen, 15-Aug-04
SUERC UNLISTED
University of Oxford, Earth Sciences Open University, Earth and Environmental 1-Aug-04
Sciences
University of Cambridge, Earth Sciences University of Cambridge, Earth Sciences 15-Jul-04
Cardiff University, School of Earth and Ocean Cardiff University, School of Earth and Ocean 1-Jul-04
Sciences Sciences
University of Reading, Meteorology National Oceanography Centre, NERC 1-Jul-04
Strategic Research Division
University of Aberdeen, Inst of Biological and University of Aberdeen, Inst of Biological and 1-Jun-04
Environmental Sci Environmental Sci
Lancaster University, Lancaster Environment Lancaster University, Biological Sciences 1-Jun-04
Centre
University of St Andrews, Biology University of St Andrews, Biology 1-May-04
Aberystwyth University, Inst of Geography University of Bristol, Earth Sciences 1-Apr-04
and Earth Sciences
Aberystwyth University, Inst of Geography Aberystwyth University, Centre for 1-Apr-04
and Earth Sciences Glaciology (IGES)
Durham University, Geography University of Reading, Geography 23-Mar-04
Pennsylvania State University, Biology University of Oxford, Zoology 8-Mar-04
Aberystwyth University, Inst of Geography University of Leeds, Sch of Geography 1-Mar-04
and Earth Sciences
University College London, Chemistry University College London, Chemistry 1-Feb-04
University of Reading, Meteorology University of East Anglia, Mathematics 19-Jan-04
Bangor University, Sch of Biological Sciences Bangor University, Inst of Environmental 1-Jan-04
Science
Imperial College London, Department of Imperial College London, Earth Science and 1-Jan-04
Earth Sciences Engineering
University of Reading, Meteorology University of Reading, Meteorology 1-Jan-04
National Oceanography Centre, Science and National Oceanography Centre, NERC 5-Dec-03
Technology Strategic Research Division
Pennsylvania State University, Biology University of Oxford, Zoology 1-Dec-03
University of Oxford, Earth Sciences University of Oxford, Earth Sciences 1-Nov-03
National Oceanography Centre, Science and Proudman Oceanographic Laboratory, 13-Oct-03
Technology UNLISTED
National Oceanography Centre, Science and Keele University, Computer Science and 1-Oct-03
Technology Mathematics
University of Reading, Meteorology University of Reading, Meteorology 1-Oct-03
Swansea University, School of the Swansea University, Biological Sciences 25-Sep-03
Environment and Society
The University of Manchester, Mathematics The University of Manchester, Mathematics 1-Sep-03
University of Reading, Meteorology NERC Centre for Ecology and Hydrology, 1-Sep-03
NERC CEH - Wallingford
University of East Anglia, Environmental University of East Anglia, Environmental 22-Aug-03
Sciences Sciences
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 4-Aug-03
University of St Andrews, Mathematics and University of St Andrews, Mathematics and 1-Aug-03
Statistics Statistics
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 1-Aug-03
University of East Anglia, Environmental University of East Anglia, Environmental 1-Aug-03
Sciences Sciences
NERC British Antarctic Survey, Science NERC British Antarctic Survey, NERC BAS - 21-Jul-03
Programmes Cambridge
University of Cambridge, Applied Maths and University of Cambridge, Applied Maths and 1-Jul-03
Theoretical Physics Theoretical Physics
University of Southampton, School of Ocean University of Southampton, School of Ocean 1-Jul-03
and Earth Science and Earth Science
University of East Anglia, Environmental University of East Anglia, Environmental 9-Jun-03
Sciences Sciences
University of St Andrews, Biology University of St Andrews, Biology 1-Jun-03
University College London, Geography University College London, Geography 1-May-03
Midland Valley Exploration Ltd, Kingston University, Sch of Geography 1-Apr-03
Headquarters Geology & Environment
University of Cambridge, Scott Polar University of Glasgow, School of 1-Dec-02
Research Institute Geographical & Earth Sciences
Royal Holloway, Univ of London, Earth King's College London, Chemistry 1-Oct-02
Sciences
University of Bristol, Chemistry University of Birmingham, School of 1-Oct-02
Chemistry
University of York, Chemistry University of York, Chemistry 1-Oct-02
Pennsylvania State University, Biology University of Oxford, Zoology 1-Oct-02
Durham University, Biological and NERC Centre for Ecology and Hydrology, 1-Sep-02
Biomedical Sciences NERC CEH - Wallingford
Durham University, Biological and Durham University, Biological and 1-Sep-02
Biomedical Sciences Biomedical Sciences
University of Edinburgh, Sch of Geosciences Aberystwyth University, Inst of Geography 1-Sep-02
and Earth Sciences
STFC - Laboratories, Space Science & STFC - Laboratories, Space Science & 1-Aug-02
Technology (SSTD) Technology (SSTD)
University of Reading, Environmental University of Reading, Environmental 1-Jun-02
Systems Science Centre Systems Science Centre
NERC Centre for Ecology and Hydrology, NERC Centre for Ecology and Hydrology, 1-Jun-02
Harding NERC CEH - Wallingford
University of Bristol, Geographical Sciences University of Reading, Meteorology 27-May-02
Swansea University, Biological Sciences Swansea University, Biological Sciences 1-May-02
Autonomous University of Barcelona (UAB), Cardiff University, School of Earth and Ocean 24-Apr-02
InstitutdeCiencia i TecnologiaAmbientals Sciences
University of Reading, Environmental The University of Manchester, Manchester 1-Apr-02
Systems Science Centre Computing
University of Reading, Environmental STFC - Laboratories, e-Science Centre - 1-Apr-02
Systems Science Centre Daresbury
University of Cambridge, Applied Maths and University of Cambridge, Applied Maths and 1-Apr-02
Theoretical Physics Theoretical Physics
University of Leeds, Sch of Chemistry University of East Anglia, Environmental 15-Mar-02
Sciences
Swansea University, School of the Swansea University, Biological Sciences 12-Mar-02
Environment and Society
University of Reading, Environmental University of Southampton, National 12-Mar-02
Systems Science Centre Oceanography Centre Southampton
University of Oxford, Oxford Physics STFC - Laboratories, Space Science & 9-Mar-02
Technology (SSTD)
University of Southampton, School of Ocean University of Southampton, National 1-Mar-02
and Earth Science Oceanography Centre Southampton
University of Reading, Environmental Imperial College London, Earth Science and 1-Jan-02
Systems Science Centre Engineering
University of Sussex, Sch of Global Studies University of Sussex, Biology and 1-Jan-02
Environmental Science
National Oceanography Centre, Science and University of Southampton, National 22-Nov-01
Technology Oceanography Centre Southampton
University of Leeds, School of Earth and University of Leeds, School of Earth and 5-Nov-01
Environment Environment
Bangor University, Sch of Biological Sciences Bangor University, Sch of Biological Sciences 1-Nov-01
University of Reading, Environmental University of Reading, Environmental 15-Oct-01
Systems Science Centre Systems Science Centre
University of Oxford, Oxford Chemistry University of Oxford, Oxford Chemistry 1-Oct-01
University of Southampton, School of University of Southampton, School of 1-Oct-01
Chemistry Chemistry
Eberhard Karls University Tuebingen, Royal Holloway, Univ of London, Earth 12-Sep-01
UNLISTED Sciences
University of Southampton, School of University of Bristol, Chemistry 1-Sep-01
Chemistry
University College London, Earth Sciences University College London, Mullard Space 20-Aug-01
Science Laboratory
National Oceanography Centre, Science and University of Southampton, National 1-Aug-01
Technology Oceanography Centre Southampton
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 20-Jul-01
University of Nottingham, Sch of Biology University of Nottingham, Sch of Biology 2-Jul-01
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 1-Jul-01
University of Cambridge, Chemistry University of Cambridge, Chemistry 1-Jul-01
University of St Andrews, Biology University of St Andrews, Biology 1-Jul-01
STFC - Laboratories, Space Science & STFC - Laboratories, Space Science & 1-Jul-01
Technology (SSTD) Technology (SSTD)
University College London, Earth Sciences University College London, Earth Sciences 11-Jun-01
Bangor University, Sch of Environment and Bangor University, Inst of Environmental 1-May-01
Natural Resources Science
University College London, Geography University College London, Geography 1-Apr-01
University of East Anglia, Environmental University of East Anglia, Environmental 15-Mar-01
Sciences Sciences
University of Cambridge, Zoology The Natural History Museum, Palaeontology 1-Mar-01
University of Bristol, Chemistry University of Bristol, Chemistry 19-Feb-01
University of Cambridge, Scott Polar University of Bristol, Geographical Sciences 1-Feb-01
Research Institute
University of Sheffield, Geography University of East Anglia, Environmental 1-Feb-01
Sciences
University of Southampton, School of Ocean University of Southampton, School of Ocean 8-Jan-01
and Earth Science and Earth Science
University of Cambridge, Zoology University of Cambridge, Zoology 1-Dec-00
University of Bristol, Geographical Sciences University of Nottingham, Sch of Biosciences 1-Dec-00
NERC British Antarctic Survey, Science NERC British Antarctic Survey, NERC BAS - 1-Dec-00
Programmes Cambridge
University of Saskatchewan, Geography Aberystwyth University, Inst of Geography 1-Nov-00
and Earth Sciences
University of Cambridge, Earth Sciences University of Cambridge, Earth Sciences 1-Oct-00
University of Edinburgh, Sch of Mathematics University of Edinburgh, Sch of Geosciences 1-Oct-00
National Oceanography Centre, Science and Keele University, Computer Science and 1-Sep-00
Technology Mathematics
University of Cambridge, Chemistry University of Cambridge, Chemistry 21-Aug-00
Lancaster University, Lancaster Environment Lancaster University, Lancaster Environment 1-Aug-00
Centre Centre
Oxford Brookes University, Geology Oxford Brookes University, Sch of Life 1-Jul-00
Sciences
NERC British Antarctic Survey, Science NERC British Antarctic Survey, NERC BAS - 7-May-00
Programmes Cambridge
Queen Mary, University of London, Sch of Heriot-Watt University, Sch of Life Sciences 1-May-00
Biological and Chemical Sciences
NERC British Antarctic Survey, Science Scottish Association For Marine Science, 1-May-00
Programmes Dunstaffnage Marine Laboratory
University College London, Chemistry University College London, Chemistry 1-May-00
The University of Manchester, Earth King's College London, Life Sciences 1-Apr-00
Atmospheric and Env Sciences
Cardiff University, School of Earth and Ocean Cardiff University, School of Earth and Ocean 1-Mar-00
Sciences Sciences
University of York, Chemistry University of Leeds, Sch of Chemistry 23-Feb-00
University of Sheffield, Geography University of Sheffield, Geography 1-Feb-00
University of Nottingham, Sch of Biology University of Nottingham, Sch of Biology 1-Jan-00
University of Bristol, Geographical Sciences University of Southampton, School of 16-Nov-99
Geography
University of Leeds, School of Earth and University of Leeds, School of Earth and 5-Nov-99
Environment Environment
Swansea University, School of the Swansea University, Geography 1-Nov-99
Environment and Society
University of Cambridge, Scott Polar University of Bristol, Geographical Sciences 1-Nov-99
Research Institute
University of Dundee, Sch of Life Sciences University of Dundee, Sch of Life Sciences 18-Oct-99
University of Edinburgh, Sch of Geosciences University of Glasgow, School of 1-Oct-99
Geographical & Earth Sciences
University College London, Chemistry University College London, Chemistry 20-Sep-99
University of Cambridge, Scott Polar University of Bristol, Geographical Sciences 1-Sep-99
Research Institute
University College London, Mullard Space University College London, Mullard Space 1-Sep-99
Science Laboratory Science Laboratory
University of Bristol, Geographical Sciences University of Nottingham, Sch of Biosciences 1-Aug-99
University of Bristol, Chemistry University of Bristol, Chemistry 1-Jul-99
Royal Holloway, Univ of London, Earth Royal Holloway, Univ of London, Earth 1-Jul-99
Sciences Sciences
University College London, Earth Sciences University College London, Earth Sciences 1-Jun-99
University of Leeds, School of Earth and University of Leeds, School of Earth and 31-May-99
Environment Environment
Durham University, Geography Durham University, Geography 1-May-99
University of Leeds, School of Earth and University of Leeds, School of Earth and 1-Apr-99
Environment Environment
University of Adelaide, School of Earth & University of Oxford, Biological 1-Apr-99
Environmental Sciences Anthropology
Queen's University of Belfast, Geography Queen's University of Belfast, Geography 1-Apr-99
Archaeology and Palaeoecology Archaeology and Palaeoecology
University of Reading, Meteorology University of Reading, Meteorology 1-Apr-99
National Oceanography Centre, Science and University of Southampton, School of Ocean 24-Mar-99
Technology and Earth Science
University of East Anglia, Environmental University of East Anglia, Environmental 22-Mar-99
Sciences Sciences
University of Adelaide, School of Earth & University of Oxford, Biological 15-Mar-99
Environmental Sciences Anthropology
University of Southampton, School of University of Southampton, School of 15-Mar-99
Geography Geography
National Oceanography Centre, Science and University of Southampton, School of Ocean 19-Feb-99
Technology and Earth Science
NERC British Antarctic Survey, Science NERC British Antarctic Survey, NERC BAS - 1-Feb-99
Programmes Cambridge
University of East Anglia, Environmental University of East Anglia, Biological Sciences 1-Feb-99
Sciences
National Oceanography Centre, Science and University of Southampton, School of Ocean 1-Feb-99
Technology and Earth Science
Swansea University, School of the Aberystwyth University, Inst of Geography 18-Jan-99
Environment and Society and Earth Sciences
University of Cambridge, Scott Polar University of Bristol, Geographical Sciences 15-Jan-99
Research Institute
University of Cambridge, Applied Maths and University of Cambridge, Geography 1-Jan-99
Theoretical Physics
University of Bristol, Geographical Sciences University of Reading, Meteorology 1-Jan-99
Swansea University, School of the University of Bristol, Geographical Sciences 1-Jan-99
Environment and Society
Swansea University, School of the University of Leeds, Sch of Geography 1-Jan-99
Environment and Society
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 1-Jan-99
University of Bristol, Geographical Sciences University of Bristol, Geographical Sciences 1-Dec-98
University College London, Earth Sciences University College London, Mullard Space 1-Nov-98
Science Laboratory
NERC British Antarctic Survey, Science Scottish Association For Marine Science, 30-Sep-98
Programmes Dunstaffnage Marine Laboratory
University of Oxford, Oxford Physics University of Oxford, Oxford Physics 1-Apr-98
University of Southampton, School of Ocean University of Southampton, School of Ocean 1-Feb-98
and Earth Science and Earth Science
Scottish Association For Marine Science, NERC Centre for Ecology and Hydrology, 1-Oct-97
Scottish Association For Marine Science NERC CEH - Windermere
University of Cambridge, Applied Maths and University of Cambridge, Applied Maths and 21-Jun-97
Theoretical Physics Theoretical Physics
University College London, Chemistry University College London, Chemistry 1-Sep-96
University of Oxford, Oxford Physics University of Oxford, Oxford Physics 1-Nov-95
University of Oxford, Oxford Physics University of Oxford, Oxford Physics 1-Jun-91
Split Award
End Date Abstract (Y/N) Total Value UK £
31-Mar-13 Along the western margin of Spitsbergen, Y - Lead 148,716
where the northern extension of Gulf Stream
system conveys warm Atlantic water into
Along the Ocean, hundreds of plumes of
31-Mar-13 the Arctic western margin of Spitsbergen, Y 363,785
where the northern extension of Gulf Stream
system conveys warm Atlantic water into
the Arctic Ocean, hundreds of plumes of
bubbles of methane gas were discovered in
31-Jan-14 The burning of fossil fuels is releasing vast Y 63,281
quantities of extra carbon dioxide to the
Earth's atmosphere. Much of this stays in
the atmosphere, raising CO2 levels, but
much also leaves the atmosphere after a
31-Jan-14 See lead proposal Y 73,804
31-Jan-14 see lead proposal Y 75,116
31-Jan-14 See lead proposal. Y 78,725
31-Jan-14 See lead proposal Y 149,685
31-Dec-13 The Earth is currently undergoing the largest N 299,945
climate experiment in history. Our climate
system is in a state of change and the most
dramatic sign of that change is the shrinking
of the Arctic sea ice cover. As ice melts, less
31-Dec-13 Our work brings together two important N 881,354
areas of science and engineering: wireless
communications technology and glaciology.
Using innovative techniques currently being
developed for wireless communications to
31-Oct-13 This project will quantify the impacts of N 321,203
processes that control export of pollution
from Europe on air quality, climate and
ecosystems. These processes currently lack
observational constraint, and our
31-Oct-13 By modifying the amount of solar radiation Y - Lead 324,216
absorbed at the land surface, bright snow
and dark forests have strong influences on
weather and climate; either a decrease in
snow cover or an increase in forest cover,
31-Oct-13 The main objective of the proposed work is N 542,718
to design and build low-cost pole-based GPS
sensors, called "Javelins", that can be
installed on the surface of a glacier by
airdropping them from an aircraft. The
30-Sep-11 This aim of this project is to develop a N 81,220
miniaturised Fourier transform
spectrometer, known as a Static Imaging
Fourier Transform Spectrometer (SIFTS). This
instrument utilises a simple optical
31-Mar-12 The Arctic is changing rapidly. One of the N 62,631
clearest changes is a reduction in the extent
and thickness of summer sea ice. The loss of
ice is predicted to increase in the coming
years as a consequence of climatic warming.
30-Sep-13 The 1.7 million km2 Greenland Ice Sheet is Y 16,173
divided into a series of major drainage
basins, each typically about 50-100,000 km2
in area. Most of these basins drain into the
marine waters of fjord systems via relatively
30-Sep-13 The 1.7 million km2 Greenland Ice Sheet is Y 56,093
divided into a series of major drainage
basins, each typically about 50-100,000 km2
in area. Most of these basins drain into the
marine waters of fjord systems via relatively
30-Sep-13 See Lead Proposal Y 90,832
30-Sep-13 See lead proposal (NOCS). Y 98,958
30-Sep-13 Oceans represent 70% of Earth's surface, Y - Lead 223,493
supporting vast biodiversity and providing
major food resources for humankind. Since
the industrial revolution, the oceans have
restricted the extent of global warming by
30-Sep-13 See lead proposal Y 516,654
30-Sep-13 The burning of fossil fuels is releasing vast Y 576,052
quantities of extra carbon dioxide to the
Earth's atmosphere. Much of this stays in
the atmosphere, raising CO2 levels, but
much also leaves the atmosphere after a
30-Sep-13 The 1.7 million km2 Greenland Ice Sheet is Y - Lead 834,814
divided into a series of major drainage
basins, each typically about 50-100,000 km2
in area. Most of these basins drain into the
marine waters of fjord systems via relatively
31-Mar-14 We propose a programme of observations, Y - Lead 228,817
combined with analysis of past and ongoing
time series, to discover the magnitude of
surface pH variations at seasonal-up-to-
decadal time scales. We will address the
31-Mar-14 The Canadian Arctic Archipelago (defined N 392,707
here to include Nares Strait which borders
Greenland) is a key gateway that links the
Arctic Ocean to the Atlantic. Changes in the
flux of freshened seawater and ice through
31-Mar-14 The burning of fossil fuels is releasing vast Y - Lead 1,001,476
quantities of extra carbon dioxide to the
Earth's atmosphere. Much of this stays in
the atmosphere, raising CO2 levels, but
much also leaves the atmosphere after a
30-Sep-14 see lead proposal - Bristol Y 13,303
30-Sep-14 Background The emerging panzootic of N 81,376
amphibian chytridiomycosis has had
profound deleterious effects on
communities and ecosystems in many areas
of the world. Our research has shown that
5-Sep-11 The British Antarctic Survey (BAS) has in N 100,541
recent years developed a highly-successful
stepped-frequency phase-sensitive radar
system (pRES) based on a general-purpose
vector network analyzer (VNA). The aim was
31-Aug-13 Oxbow lakes are some of the most N 74,977
widespread and distinctive landforms along
meandering rivers of the world, functioning
as vital aquatic floodplain habitat for many
threatened species and as important sinks
31-Aug-13 See lead proposal Y 80,119
31-Aug-13 See lead proposal Y 148,647
31-Aug-13 Rapid climate change is indisputable in the N 216,065
Arctic, where the record minimum sea-ice
extent of September 2007 has been
followed by the fastest recorded rate of sea-
ice loss in August 2008 leading to near-
31-Aug-13 Some of the most iconic images of climate Y 233,343
change and sea level rise include footage of
the dramatic moment when a large
fragment of ice breaks off from the terminus
of a glacier and scenes of melting icebergs.
31-Aug-13 Some of the most iconic images of climate Y - Lead 311,960
change and sea level rise include footage of
the dramatic moment when a large
fragment of ice breaks off from the terminus
of a glacier and scenes of melting icebergs.
28-Feb-14 We propose a programme of observations, Y 137,595
combined with analysis of past and ongoing
time series, to discover the magnitude of
surface pH variations at seasonal-up-to-
decadal time scales. We will address the
31-Aug-14 See lead proposal - Bristol University Y 13,428
31-Aug-14 The Greenland Ice Sheet is the main Y - Lead 581,791
reservoir of ice in the northern hemisphere
capable of affecting sea level in the 21st
Century. Measurements of the elevation of
the ice sheet surface from aircraft now
31-Jul-11 Over the last 150 years or so the N 29,047
industrialisation of the human race has
caused the climate of our planet to change.
The principal causes of this change are our
emissions of greenhouse gases such as
31-Jul-13 The Arctic is a region of extreme sensitivity N 316,658
to climate change. Observations show its
temperature to be increasing at twice the
rate of the rest of the world. Models suggest
this strong response will continue; however
31-Jul-13 Tropical ecosystems are major sources of Y - Lead 395,440
the greenhouse gases (GHGs) methane (CH4)
and nitrous oxide (N2O), which are 25 and
298 times more effective than carbon
dioxide (CO2), respectively, in trapping long-
31-Jul-13 There is a long-standing 'chicken and egg' N 469,576
debate over rifting and the injection of
molten rock into the crust at rifted spreading
centres: does the molten rock injection drive
rifting or vice-versa? A further question is
30-Jun-12 Many sub-surface environments currently N 185,831
feature as "voids" in our understanding of
the Earth's system, because inaccessibility
and hostile conditions prevent the use of
cabled measurement devices. The basal
30-Jun-13 Tropical ecosystems are major sources of Y 38,316
the greenhouse gases (GHGs) methane (CH4)
and nitrous oxide (N2O), which are 25 and
298 times more effective than carbon
dioxide (CO2), respectively, in trapping long-
19-Dec-10 The 14 April-ongoing 2010 explosive N 51,551
eruption at Eyjafjöll volcano, south Iceland
unexpectedly caused widespread disruption
to aviation and every day life in the UK and
Europe, resulting in economic difficulties
13-Dec-13 Although life successfully moderates surface Y 25,951
conditions on Earth, some events in Earth
History have threatened the viability of most
life forms. Arguably the most profound and
long-lasting challenge in the last 2 billion
9-Jun-11 The Earth's energy balance is in equilibrium, N 112,017
that is to say, an equal amount of energy is
absorbed and emitted, The Sun is the source
of all energy for the Earth, heating the planet
via sunlight, warming the surface and this
31-May-11 The response of the Greenland Ice Sheet to a N 41,703
warming climate is of great significance for
models of sea-level rise. As such, it receives
significant attention from the media, among
the general public and in government policy
31-May-11 Brittle fractures and faults are the most N 63,266
common expression of deformation at the
Earth's surface. Well known examples
include the famous San-Andreas-Fault
(California, USA) or North-Anatolian-Fault (N
30-Nov-13 We propose a programme of observations, Y 153,866
combined with analysis of past and ongoing
time series, to discover the magnitude of
surface pH variations at seasonal-up-to-
decadal time scales. We will address the
16-May-13 Waves in the atmosphere are able to Y - Lead 376,349
transport energy and momentum between
different layers of the atmosphere.
Understanding these waves is thus very
important if we want to understand the
31-Dec-10 One of the most prominent signatures of N 53,191
climate change is progressively increasing
levels of atmospheric methane (CH4).
Although atmospheric carbon dioxide (CO2)
levels are higher than CH4, CH4 has
30-Jun-11 There are a number of distinct types of data Y - Lead 85,434
which environmental scientists use to study
the Earth - in-situ data, remotely-sensed
data and numerical model output. There
needs to be greater integration of these
30-Apr-13 Submarine channels are spectacular features Y - Lead 311,864
that can extend for thousands of kilometres
across the seafloor, are often kilometres
wide and up to hundreds of metres deep.
They are formed by density currents;
8-Apr-13 The importance and relevance of N 429,488
communicating our knowledge of future
climate has never been more widely
recognised, and needs no further
introduction here. Yet both the Stern report,
7-Apr-11 The Labrador and Nordic Seas are key N 64,385
elements in the global climate system. They
are the main sites for dense water formation
at the northern limit of the global ocean
circulation and are experiencing major
31-Mar-11 We want to build a scientific instrument that N 146,683
can measure the amount of algae growing
on the underside of sea ice. Sea-ice algae
form the base of many polar marine
foodwebs, but data on the mesoscale (tens
31-Mar-12 Peatlands are the largest natural sources of N 65,205
the greenhouse gas methane (CH4), and
understanding the potential contributions of
peatlands to atmospheric CH4 budgets is
crucial for understanding current and future
31-May-12 The anthropogenic burning of fossil fuels is Y 351,415
affecting the climate system via raised
atmospheric CO2 concentrations. But are
there aspects of the natural Earth system
that, when forced by imposed climate
30-Sep-12 Past terrestrial responses to climate-ocean Y 10,028
interactions in the North Atlantic region are
a critical research priority because they
show how changes in key aspects of climate
that will be affected by future global
30-Sep-12 Past terrestrial responses to climate-ocean Y 125,380
interactions in the North Atlantic region are
a critical research priority because they
show how changes in key aspects of climate
that will be affected by future global
30-Sep-12 Past terrestrial responses to climate-ocean Y - Lead 194,877
interactions in the North Atlantic region are
a critical research priority because they
show how changes in key aspects of climate
that will be affected by future global
31-Mar-13 Waves in the atmosphere are able to Y 90,225
transport energy and momentum between
different layers of the atmosphere.
Understanding these waves is thus very
important if we want to understand the
31-Mar-13 The anthropogenic burning of fossil fuels is Y - Lead 265,370
affecting the climate system via raised
atmospheric CO2 concentrations. But are
there aspects of the natural Earth system
that, when forced by imposed climate
31-Mar-13 Tropical ecosystems are major sources of Y 358,391
the greenhouse gases (GHGs) methane (CH4)
and nitrous oxide (N2O), which are 25 and
298 times more effective than carbon
dioxide (CO2), respectively, in trapping long-
30-Sep-13 Although life successfully moderates surface Y 124,791
conditions on Earth, some events in Earth
History have threatened the viability of most
life forms. Arguably the most profound and
long-lasting challenge in the last 2 billion
30-Sep-13 Although life successfully moderates surface Y - Lead 644,767
conditions on Earth, some events in Earth
History have threatened the viability of most
life forms. Arguably the most profound and
long-lasting challenge in the last 2 billion
22-Feb-12 The geomagnetic field is a fundamental and Y 20,625
very useful property of the Earth, both in
practical terms (for navigation, industrial
applications and resource exploration) and in
academic terms, for what it can tell us about
15-Feb-12 The ice is melting! Between 1979 and 2007 Y - Lead 31,772
the summer sea ice extent in the Arctic has
halved, from over 8 million square km to just
over 4 million square km. Moreover,
measurements from submarines suggest
14-Feb-12 The geomagnetic field is a fundamental and Y - Lead 179,023
very useful property of the Earth, both in
practical terms (for navigation, industrial
applications and resource exploration) and in
academic terms, for what it can tell us about
14-Feb-13 Currently there is major uncertainty Y - Lead 322,257
surrounding the contributions of the
Greenland and Antarctic ice sheets to future
sea level rise. The majority of the ice
discharged by these ice sheets into the
10-Feb-13 The Arctic is one of the most vulnerable Y 26,292
regions on Earth and there is clear evidence
that its ecosystems are changing rapidly.
These changes are generally attributed to
recent global warming, the effects of which
4-Aug-11 The last glacial period was punctuated by Y 32,092
repeated, large, millennial-scale (hundreds
to thousands of years) shifts in northern
hemisphere climate known as Dansgaard-
Oeschger (D-O) oscillations. These events
31-Jan-11 SUMMARY: The background for this proposal N 50,847
originates from scientific fieldwork
performed by the proposer on the sea ice
around the Qaanaaq region (NW Greenland)
in the spring of 2008. The aim of this climate-
31-May-11 Our Aim This project aims to develop and Y 25,520
design a new satellite mission. This new
mission concept will be a spaceborne multi-
spectral canopy lidar (called SpeCL,
"speckle") that can measure the vertical
31-May-11 Our Aim This project aims to develop and Y - Lead 153,960
design a new satellite mission. This new
mission concept will be a spaceborne multi-
spectral canopy lidar (called SpeCL,
"speckle") that can measure the vertical
31-Jan-12 ESA is due to launch the three-satellite N 189,855
mission, SWARM, in 2010 as part of its Earth
Explorer programme, which is strategic for
the geomagnetic element of Earth
Observation. The planned multi-spacecraft
31-Jan-13 PROJECT SUMMARY As a result of N 91,863
continuous burning of fossil fuel, the global
environment is facing a crisis stemming from
rapidly rising concentrations of carbon
dioxide and other greenhouse gases in our
13-Jan-13 More than 99.8% of living vertebrates are Y 127,412
gnathostomes (vertebrates with jaws and
teeth), and the origin of gnathostomes thus
represents one of the most significant
episodes in animal evolution. Teeth and jaws
6-Jan-12 The ice is melting! Between 1979 and 2007 Y 37,244
the summer sea ice extent in the Arctic has
halved, from over 8 million square km to just
over 4 million square km. Moreover,
measurements from submarines suggest
3-Jan-13 It is very important for us to find out how Y 77,243
climate changed in the past. Without
knowing, we cannot predict how the future
climate might behave. Global, systematic
measurements of climatic variables have
3-Jan-13 It is very important for us to find out how Y - Lead 321,639
climate changed in the past. Without
knowing, we cannot predict how the future
climate might behave. Global, systematic
measurements of climatic variables have
31-Mar-10 Understanding the evolution and dynamics N 11,878
of the Antarctic cryosphere, from its
inception during the Eocene-Oligocene
transition (~33 Ma) through the significant
periods of climate change during the
31-Dec-12 The Arctic is one of the most vulnerable Y 27,297
regions on Earth and there is clear evidence
that its ecosystems are changing rapidly.
These changes are generally attributed to
recent global warming, the effects of which
31-Dec-12 There is now unambiguous evidence that Y 166,950
ecosystems in the Arctic are changing. This is
generally attributed to global warming,
effects of which are particularly enhanced in
this region. In this project we will test the
31-Dec-12 The Arctic is one of the most vulnerable Y - Lead 253,218
regions on Earth and there is clear evidence
that its ecosystems are changing rapidly.
These changes are generally attributed to
recent global warming, the effects of which
31-Dec-12 Microscopic plants, or phytoplankton, use N 286,347
the sun's energy to combine atmospheric
carbon dioxide (CO2) and water to produce
particulate organic matter (POM). A
proportion of this sinks to the seabed, where
31-May-11 The changes to the Greenland and Antarctic N 159,022
Ice Sheets are spectacular manifestations of
global climate change. Greenland has seen
recent accelerated changes across large
outlet glaciers, whilst glaciers in West
18-Oct-13 North west Europe has a relatively mild Y 317,139
climate in part because of heat pulled north
through the Atlantic by the overturning.
There is a risk that global warming will cause
this circulation to rapidly decrease with
30-Sep-12 Currently there is major uncertainty Y 8,713
surrounding the contributions of the
Greenland and Antarctic ice sheets to future
sea level rise. The majority of the ice
discharged by these ice sheets into the
30-Sep-12 More than 99.8% of living vertebrates are Y - Lead 320,305
gnathostomes (vertebrates with jaws and
teeth), and the origin of gnathostomes thus
represents one of the most significant
episodes in animal evolution. Teeth and jaws
22-Sep-12 The Eemian interglacial serves as the most Y 20,453
recent analogue for understanding the
natural operation of the climate system
during the current interglacial. The nature
and pattern of the full deglaciation cycle and
22-Nov-13 North west Europe has a relatively mild Y 250,158
climate in part because of heat pulled north
through the Atlantic by the overturning.
There is a risk that global warming will cause
this circulation to rapidly decrease with
31-Aug-11 N 73,823
31-Aug-11 N 135,708
31-Aug-12 The Eemian interglacial serves as the most Y 97,414
recent analogue for understanding the
natural operation of the climate system
during the current interglacial. The nature
and pattern of the full deglaciation cycle and
31-Aug-12 Summary An increasing number of scientific Y 115,325
studies show that human activities, e.g.
burning of fossil fuels, have increased the
concentration of heat-trapping gasses in the
atmosphere. It is estimated that global
27-Aug-12 An increasing number of scientific studies Y 93,018
show that human activities, e.g. burning of
fossil fuels, have increased the concentration
of heat-trapping gasses in the atmosphere. It
is estimated that global temperatures will
13-Jul-13 The National Centre for Atmospheric Science N 153,409
(NCAS) will coordinate the NERC Earth
System Science Graduate School (NESSGS)
on behalf of a consortium of NERC Research
and Collaborative Centres and strong
30-Jun-10 We propose a detailed study of the biotic N 34,359
record (foraminifera and calcareous
nannofossils) of the Eocene/Oligocene
transition in ODP Hole 647 in the Labrador
Sea. The sediments in this core constitutes
30-Jun-11 It has long been known that the biological N 23,205
activity of the oceans is regulated by the
availability of the major nutrient ions
phosphate, nitrate, and silicate. More
recently, however, it has been recognized
25-Dec-10 The Greenland ice sheet, and its current and N 39,899
future contribution to sea level rise, has
attracted a great deal of attention from
scientists, media, public and policy makers.
This has arisen because recent results show
21-Jun-12 This project uses two novel inputs to address N 334,353
the fundamental problem of understanding
observed variability and change in the
Atlantic Ocean in the context of the global
coupled atmosphere-ocean system. Using a
31-May-11 The body of scientific evidence for significant N 53,057
anthropogenic impacts on the global climate
is growing and public concern underscores a
need for better assessments of
contemporary environmental changes in
31-Jul-11 The last glacial period was punctuated by Y - Lead 106,541
repeated, large, millennial-scale (hundreds
to thousands of years) shifts in northern
hemisphere climate known as Dansgaard-
Oeschger (D-O) oscillations. These events
30-May-12 The Eemian interglacial serves as the most Y - Lead 231,131
recent analogue for understanding the
natural operation of the climate system
during the current interglacial. The nature
and pattern of the full deglaciation cycle and
27-Jul-13 North west Europe has a relatively mild Y - Lead 317,008
climate in part because of heat pulled north
through the Atlantic by the overturning.
There is a risk that global warming will cause
this circulation to rapidly decrease with
4-Nov-14 This project addresses the current Y - Lead 456,789
uncertainty in the present-day contribution
of the West Antarctic Ice Sheet to global sea
level rise. These estimates are primarily
derived from space geodetic (altimetry or
30-Apr-12 Copepods are free-drifting animal plankton Y - Lead 259,973
found throughout the ocean in vast
numbers. This group plays a critical role in
the biochemistry of the upper ocean. They
are the dominant grazers of many
30-Apr-14 North west Europe has a relatively mild Y 315,090
climate in part because of heat pulled north
through the Atlantic by the overturning.
There is a risk that global warming will cause
this circulation to rapidly decrease with
6-Apr-12 An increasing number of scientific studies Y - Lead 261,519
show that human activities, e.g. burning of
fossil fuels, have increased the concentration
of heat-trapping gasses in the atmosphere. It
is estimated that global temperatures will
31-Mar-12 Copepods are free-drifting animal plankton Y 22,061
found throughout the ocean in vast
numbers. This group plays a critical role in
the biochemistry of the upper ocean. They
are the dominant grazers of many
31-Mar-12 Life exists whatever there is water and Y 184,563
glaciers are no exception. Indeed glaciers are
vast reservoirs of biological cells and debris.
The debris can cover ca 1-10% of the surface
of glaciers worldwide, and it is composed of
1-Jul-09 As more people today become concerned N 244,152
about global warming and the effect that
humans are having on the climate, it
becomes more important for people to
understand what the climate and
31-Jul-11 The stratospheric ozone layer, located Y 77,579
between altitudes of approximately 15 and
40 km, performs a number of critical roles in
the Earth's atmosphere: It shields the
biosphere from harmful UV radiation,
29-Feb-12 Life exists whatever there is water and Y - Lead 413,977
glaciers are no exception. Indeed glaciers are
vast reservoirs of biological cells and debris.
The debris can cover ca 1-10% of the surface
of glaciers worldwide, and it is composed of
8-Jan-11 The chemical evolution of the oceans is N 26,701
fundamentally tied to climate change and
biological evolution throughout Earth
history. Few methods exist for directly
reconstructing the past ionic composition of
30-Sep-10 Many processes that influence surface N 26,465
climate have their origins in the
stratosphere, the layer of the atmosphere 15-
40km above the ground. For instance, ozone
changes caused by changes in solar output
31-Jul-11 The stratospheric ozone layer, located Y - Lead 325,594
between altitudes of approximately 15 and
40 km, performs a number of critical roles in
the Earth's atmosphere: It shields the
biosphere from harmful UV radiation,
18-Jan-12 This proposal concerns the present-day N 278,590
contributors to global and regional sea level
change. Changes in sea level will not be the
same world-wide, because the ocean must
respond gravitationally to the changes in
4-Jan-10 Heinrich events, named after Hartmut N 37,579
Heinrich who first described them in 1988,
are layers of ice rafted debris (IRD) found in
North Atlantic sediment cores dating to the
last glaciation. They are believed to have
4-Jan-12 This project will quantify the effect of Y 203,972
surface generated melt-water fluctuations
on ice motion at the margin of the
Greenland Ice Sheet (GrIS). More specifically,
it will provide data that will enable ice-sheet
30-Jun-09 Single-celled grazers (protists) form a key N 40,426
trophic link between organisms at the base
of the marine food web (bacteria &
phytoplankton) and larger planktonic
predators (zooplankton). Many of these
31-Mar-11 Currently the polar regions are exhibit the N 38,126
greatest amount of warming of any region
on the planet, a feature which is not well
produced in any of the current generation of
climate models. The potential response of
31-Dec-11 This project will quantify the effect of Y - Lead 222,231
surface generated melt-water fluctuations
on ice motion at the margin of the
Greenland Ice Sheet (GrIS). More specifically,
it will provide data that will enable ice-sheet
31-Dec-11 An aerosol particle is so small that you could N 287,946
line up one hundred in the width of a human
hair. It can float in the air almost
undetected. These particles are important
for human health: for example pollen causes
30-Nov-11 The interaction between the marine and N 391,592
atmospheric carbon cycle is a critical factor
in understanding climate change. The polar
oceans play an important role in mediating
the Earth's climate, for example, by
30-Apr-11 The ice is melting! Between 1979 and 2007 N 76,932
the summer sea ice extent in the Arctic has
halved, from over 8 million square km to just
over 4 million square km. Moreover,
measurements from submarines suggest
30-Sep-10 ABSTRACT The PI proposes to undertake, as N 47,594
part of an international polar campaign, a
fieldtrip to Barrow (Alaska) in the Arctic
where he will characterize the visible optical
properties of snowpack and sea-ice and use
31-Mar-11 Long distance migration in birds is one of the N 298,455
world's most astonishing wildlife spectacles
and has puzzled humans for since the time
of Aristotle. However despite this long
standing interest and many years of study
31-May-11 This project is designed to determine the N 221,389
active methane sources in the Arctic by
measurement of d13C(CH4) at several key
sites, and by trajectory modelling studies to
identify the location, nature and seasonality
30-Sep-11 In mammals, mothers provide the resources N 302,682
and early environment in which young
develop and are thus the most influential
factor determining individual phenotypes.
Individual development is the result of own
31-Mar-12 Sea level rise is one of the few undisputed N 411,347
elements of future climate change to which
we are already committed regardless of
future emissions scenario. Projections for
regional sea level change over the next
31-Mar-12 An international effort is underway to drill a N 420,214
new ice core in Greenland: the North
Greenland Eemian Ice Drilling project
(NEEM). This presents an exciting and rare
opportunity to obtain "firn" air and ice cores
30-Sep-12 This project brings together aerosol N 64,343
modelling expertise at the University of
Leeds with climate modelling expertise at
the Met Office to tackle the pressing
problem of air pollition-climate interactions
30-Sep-12 Sea level rise (SLR) is considered to be one of N 64,343
the most economically and socially
important consequences of global warming.
The potential contribution of the ice sheets
dominates uncertainties in projections of
30-Sep-12 This project will address a significant part of N 65,487
the global climate system. The overflow of
cold, dense water from the Nordic Seas to
the Atlantic Ocean across the Greenland-
Scotland Ridge is an important component
30-Sep-12 The Arctic is a region of exceptional N 65,903
sensitivity to climate change: the observed
rate of temperature increase is twice that of
the rest of the world, and there is strong
evidence for thinning and retreat of Arctic
30-Sep-12 The Sir Alister Hardy Foundation for Ocean N 71,343
Science (SAHFOS) maintains and continually
extends their records from the Continuous
Plankton Recorder (CPR) survey, one of the
longest and richest marine monitoring
30-Sep-12 This project relates to the priority topic in N 74,568
SOFI theme 1, "Climate, ..", "Parametrisation
of detailed sea ice physics to be suitable for
ocean GCMs (studentship; WP 1.8 also WP
9.1-9.4)." Rapid changes have been observed
30-Sep-12 Improved understanding of the ocean's N 75,030
biological carbon pump and the possible
influence of ocean acidification on the
effectiveness of this pump are key issues in
climate change research. This proposed SOFI
30-Sep-12 AIM: The student will specifically test the N 80,985
hypothesis that, M. marshalli, a gastro-
intestinal nematode that infects reindeer
over winter when are nutritionally stressed,
depresses host performance and ultimately
31-Aug-11 There is a consensus: the Arctic Ocean faces N 86,197
a future with less sea ice. Therefore more
sunlight reaches the surface waters
accompanied with major implications for the
ecosystem functioning, productivity, and
31-Jul-11 Marine phytoplankton play a central role in Y - Lead 289,667
the cycling of biologically important
elements, such as carbon (C), nitrogen (N)
and phosphorous (P) between the
atmosphere, ocean and marine sediments.
31-Mar-09 The climate is warming. The Arctic regions of N 62,205
the world have been shown to be warming
at a rate faster than any other region on
earth. These high northern latitude regions
may play a critical role in determining the
30-Jun-10 One third of the global soil carbon is stored N 55,531
in northern peatlands. Today, the organic
carbon stored in peatlands in permafrost
regions, is under threat from climate
warming. If the decomposition rates of the
27-Nov-10 The Antarctic is a uniquely important Y - Lead 200,158
'natural laboratory' for examining ecosystem
responses to climate change, and it is vital
that the biological changes being observed
there are properly understood. Its
31-Jan-10 Organism responses to changing N 245,416
environments are currently primarily
addressed using two divergent approaches.
There are observational studies of range and
changes in range of species and secondly
30-Apr-09 Diel vertical migration (DVM) by zooplankton N 67,619
is a prominent feature of many marine
ecosystems. Animals move quickly tens to
hundreds of meters vertically around dawn
and dusk in migrations that comprise the
30-Apr-11 The widely publicised rapid disintegrations of Y - Lead 374,389
the Larsen A and B ice shelves on the
Antarctic Peninsula in 1995 and 2002 were
extraordinary demonstrations of the
dramatic impact that climatic changes can
30-Jun-09 Common experience with the day-to-day N 54,548
weather reveals that the presence or
absence of clouds has a profound impact on
surface temperature, by the way clouds
block the incoming radiation from the sun
31-Mar-10 In order to predict the consequences of Y 15,673
global warming, it is essential to understand
the climate response in terms of
temperature and ice volume (hence sea
level) to atmospheric carbon dioxide. The
31-Jan-11 Almost half of the Earth's carbon is stored in Y 275,041
gas hydrates and related shallow gas
deposits. Numerical models predict that this
reservoir is highly mobile and that escaping
gas has a significant potential to accelerate
28-Feb-11 Large areas of the floor of the oceans are N 329,979
draped with sediment chiefly composed of
biogenic calcium carbonate, the remains of
calcareous organisms (foraminifera,
coccolithophores, pteropods) whose shells
31-Mar-11 In order to predict the consequences of Y 23,796
global warming, it is essential to understand
the climate response in terms of
temperature and ice volume (hence sea
level) to atmospheric carbon dioxide. The
31-Mar-11 The exchange of water between the Nordic Y 136,844
Seas and the North Atlantic Ocean is part of
the global thermo-haline circulation in which
warm, saline water flows northwards in the
near/surface layers while cold fresher water
31-Mar-11 In order to predict the consequences of Y 151,384
global warming, it is essential to understand
the climate response in terms of
temperature and ice volume (hence sea
level) to atmospheric carbon dioxide. The
31-Mar-11 The exchange of water between the Nordic Y - Lead 174,101
Seas and the North Atlantic Ocean is part of
the global thermo-haline circulation in which
warm, saline water flows northwards in the
near/surface layers while cold fresher water
31-Mar-11 In order to predict the consequences of Y - Lead 360,036
global warming, it is essential to understand
the climate response in terms of
temperature and ice volume (hence sea
level) to atmospheric carbon dioxide. The
18-Sep-09 The body of scientific evidence for significant N 53,258
anthropogenic impacts on the global climate
is growing and public concern underscores a
need for better assessments of
contemporary environmental changes in
4-Sep-11 The rate at which ice flows into the sea from N 253,840
the large ice-sheets directly affects sea-level.
The forces which drive this flow are
controlled by the increasingly well-known
geometry of the the ice-sheets, but the
28-Feb-11 Look at a map of the world and find the Y 166,857
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
28-Feb-11 Methane is a strong greenhouse gas N 376,860
produced in sediments directly from
microorganisms, or from prolonged heating
of fossil carbon. Release of methane to the
ocean and atmosphere is known to have
19-Sep-08 In late 2007, the European Space Agency's N 25,525
first Earth Explorer mission will be launched.
The Gravity field and steady-state Ocean
Circulation Explorer (GOCE) mission, is
focused on the determination of a high
31-Jan-11 Velocity profiles of the Earth's upper mantle N 71,608
are characterized by discontinuous jumps of
the seismic velocities. The main velocity
discontinuities (or simply discontinuities) are
located at depths of approximately 410 and
31-Dec-10 Almost half of the Earth's carbon is stored in Y 170,993
gas hydrates and related shallow gas
deposits. Numerical models predict that this
reservoir is highly mobile and that escaping
gas has a significant potential to accelerate
31-Dec-10 Iceland represents a natural laboratory for N 389,324
studying the colonization of freshwater
habitats by fish since rivers and lakes all date
from the end of the last Ice-Age less than
10,000 years ago. The North Atlantic
14-Nov-10 Look at a map of the world and find the Y 86,445
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
30-Oct-09 The COBRA (Impact of combined iodine and N 27,279
bromine release on the Arctic atmosphere)
consortium project is already funded via an
International Polar Year (IPY) grant, with the
main objectives of improving the
14-Jan-11 Satellite and submarine observations reveal N 422,481
the Arctic sea ice cover is thinning at a rapid
rate. Recent computer modelling shows that
predictions of sea ice export into the
Greenland Sea, where it will melt to form a
31-Mar-11 Carbon is one of the essential elements N 445,342
required for life to exist, alongside energy
and liquid water. In contrast to other parts
of the Earth's biosphere, cycling of carbon
compounds beneath glaciers and ice sheets
31-Aug-10 On June 15 2006, the World Wildlife N 324,556
Federation (WWF) released a report called
'Killing them Softly', which highlighted
concern over the accumulation and toxic
effects of persistent organic pollutants
19-Feb-10 The Arctic is one of the most sensitive N 76,218
regions on Earth to climate change.
Observations show it to be warming at twice
the rate of the rest of the world. Climate
models suggest this is due to a stronger
29-Jul-10 Summary Small particles play several very Y 69,567
important roles in the atmosphere. They
provide surfaces on which exotic chemical
reactions can take place, and they act as the
condensation nuclei ("seeds") on which
29-Jul-10 Look at a map of the world and find the Y 135,416
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
1-Aug-11 Recent observations from around the Y - Lead 252,205
Greenland Ice Sheet have shown that the
fast flowing glaciers - "ice streams" - which
drain the ice sheet into the sea are thinning,
speeding up and in some cases their floating
20-Jun-09 What would happen if ocean circulation N 68,851
slowed or stopped? It is certain that in
western Europe there would be substantial
and potentially catastrophic economic and
environmental collapse. What is required to
19-Jun-10 The largest earthquakes (e.g. Chile, 1960; N 20,181
Andaman-Sumatra, 2004) are generated at
convergent plate boundaries, where oceanic
plates subduct beneath other tectonic
plates. During plate convergent, large
31-Aug-08 Outbreaks of human pathogens such as Y 4,150
Escherichia coli O157 (E. coli) attract media
attention due to the potentially severe
threat to health and life. Contaminated food
is not the only source of infection. Microbial
31-May-09 It is well known that the equatorial ocean- N 191,652
atmosphere system plays a key role in global
climate events such as the El Nino-Southern
Oscillation (ENSO) phenomenon. There is
now compelling evidence that changes in the
31-Mar-11 Look at a map of the world and find the Y 196,137
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
31-Mar-11 Look at a map of the world and find the Y 293,870
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
31-Mar-11 Look at a map of the world and find the Y - Lead 695,883
Shetland Islands. Follow the 60 degrees
north latitude circle eastwards. You pass
through St. Petersburg, the Ural Mountains,
Siberia, the Bering Sea, Alaska, northern
9-Apr-10 Polar sunrise ozone and mercury depletion Y 137,312
events are yearly phenomena that occur
throughout the Arctic and Antarctic coastal
regions, and have implications for the
atmospheric oxidative capacity, climate and
4-Apr-09 Natural diamonds are formed at high N 30,529
pressures and temperatures deep within the
Earth's interior. When diamonds form,
probably from carbonate-rich fluids in the
mantle, they sometimes encapsulate small
31-Dec-08 Outbreaks of human pathogens such as Y - Lead 58,258
Escherichia coli O157 (E. coli) attract media
attention due to the potentially severe
threat to health and life. Contaminated food
is not the only source of infection. Microbial
30-Apr-10 Predation is a key factor in the structuring of Y - Lead 289,409
ecological populations and communities. The
behavioural adaptations of predators and
prey to each other can have a fundamental
effect on population processes by affecting
31-Dec-10 Polar sunrise ozone and mercury depletion Y 87,768
events are yearly phenomena that occur
throughout the Arctic and Antarctic coastal
regions, and have implications for the
atmospheric oxidative capacity, climate and
28-Dec-10 Polar sunrise ozone and mercury depletion Y - Lead 226,407
events are yearly phenomena that occur
throughout the Arctic and Antarctic coastal
regions, and have implications for the
atmospheric oxidative capacity, climate and
18-Mar-10 Polar sunrise ozone and mercury depletion Y 58,560
events are yearly phenomena that occur
throughout the Arctic and Antarctic coastal
regions, and have implications for the
atmospheric oxidative capacity, climate and
29-Feb-08 It is widely acknowledged that the oceans N 38,671
and polar sea-ice play critical roles in global
climate change. As such, sea surface
temperature and polar sea-ice
reconstruction should be of paramount
28-Feb-10 The surface of the Earth is continually N 341,069
changing due to convection in the mantle
and the movement of rigid plates
(lithosphere) across its surface. Throughout
Earth history the continents have been
30-Apr-11 Over the past thirty years, the westerly N 259,327
winds blowing around the Southern Ocean
have grown stronger, and this change in the
circulation of the atmosphere has led to a
cooling over most of Antarctica, and a
31-Jul-10 Small particles play several very important Y - Lead 594,900
roles in the atmosphere. They provide
surfaces on which exotic chemical reactions
can take place, and they act as the
condensation nuclei ("seeds") on which
31-Jul-11 Recent observations from around the Y 217,341
Greenland Ice Sheet have shown that the
fast flowing glaciers - "ice streams" - which
drain the ice sheet into the sea are thinning,
speeding up and in some cases their floating
31-Dec-08 Floods in the UK are often caused by heavy N 192,175
rainfall lasting from minutes to weeks.
Houses in flat areas are particularly at risk:
meeting the shortage of houses in the south-
east requires building on these areas. To
31-Dec-10 Almost half of the Earth's carbon is stored in Y 174,038
gas hydrates and related shallow gas
deposits. Numerical models predict that this
reservoir is highly mobile and that escaping
gas has a significant potential to accelerate
31-May-08 Currently, the Greenland ice sheet is N 95,800
undergoing rapid changes in the coastal
regions which have been attributed to a
general warming trend to the regions
climate over the last decade. Several of the
28-Feb-10 When ice sheets flow across the landscape Y 216,380
they often produce particular landforms, the
best known of which are drumlins. These are
elongate streamlined hills, kilometres in
length and tens of metres in height. Mega-
27-Mar-10 It is widely acknowledged that polar sea-ice N 333,012
plays a critical role in global climate change.
As such, sea-ice reconstruction should be of
paramount importance in establishing
climatic evolution of the geological past.
14-May-10 SOLAS (Surface Ocean - Lower Atmosphere N 232,916
Study) is a large international research
programme whose aim is to the quantify the
exchange of gases and particles between the
ocean and the atmosphere and to
31-Oct-10 Climate warming is resulting from disruption Y 204,594
of the global carbon cycle. The Arctic is
already warming significantly, and warming
is expected to be fastest and greatest at high
latitudes, 4-7 degrees C over the next
30-Jun-10 To make the best use of the historical Y 30,360
research ship records as well as new
observations from autonomous ocean
profiling floats and special observing
programs such as Rapid climate change, it is
13-Mar-10 When ice sheets flow across the landscape Y - Lead 196,619
they often produce particular landforms, the
best known of which are drumlins. These are
elongate streamlined hills, kilometres in
length and tens of metres in height. Mega-
31-Aug-09 The course is designed to attract physical N 195,894
science and mathematics graduates into
Environmental Science and train them for a
research career. The course provides them
with a broad overview of physical problems
31-Aug-11 The primary aims of this research-led N 124,561
masters course are to provide advanced
training in the theory and techniques by
which diverse kinds of spatio-temporal data
can be processed into new knowledge, and
31-Aug-08 Interpreting past environmental change N 34,450
from lake sediments is becoming
increasingly important for understanding
past, present and future global change. In
order to understand rates of environmental
31-Mar-10 Greenland has a major influence on the Y 29,178
atmospheric circulation of the North Atlantic-
Western Europe region; dictating the
location and strength of mesoscale (100-km
scale) weather systems around the coastal
30-Jun-07 Sea ice is found in frozen polar seas and N 64,459
covers approximately 13% of the Earth's
surface. As seawater freezes, the salt
present in the water becomes concentrated
as brines within channels in the sea ice.
30-Jun-09 Climate warming is resulting from disruption Y 191,964
of the global carbon cycle. The Arctic is
already warming significantly, and warming
is expected to be fastest and greatest at high
latitudes, 4-7 degrees C over the next
5-Jan-10 Polar regions are strong indicators of the Y 123,305
impact of environmental factors upon global
climate, as indicated by the Antarctic ozone
hole, by large temperature increases on the
Antarctic Peninsula, and by Arctic sea ice
4-Dec-09 The role of ocean circulation during global N 226,756
climate changes that occur during glacial-
interglacial cycles and on millenial timescales
has been the subject of intense research.
Ocean circulation redistributes heat on the
31-May-09 Climate warming is resulting from disruption Y 190,199
of the global carbon cycle. The Arctic is
already warming significantly, and warming
is expected to be fastest and greatest at high
latitudes, 4-7 degrees C over the next
31-Jul-09 Climate warming is resulting from disruption Y 211,251
of the global carbon cycle. The Arctic is
already warming significantly, and warming
is expected to be fastest and greatest at high
latitudes, 4-7 degrees C over the next
28-May-09 Just like humans, algae are plagued by N 50,313
diseases caused by fungi, bacteria or viruses.
This is of ecological importance since entire
populations can be periodically decimated,
or impacted in a variety of other ways. Also
31-Oct-07 Current attempts to interpret the effects of N 30,919
global climate change hinge on the analysis
of ice and sediment cores from places such
as Greenland, Antarctica and the North
Atlantic. However, while these records are
30-Apr-09 Climate warming is resulting from disruption Y 89,475
of the global carbon cycle. The Arctic is
already warming significantly, and warming
is expected to be fastest and greatest at high
latitudes, 4-7 degrees C over the next
31-Jan-10 Polar regions are strong indicators of the Y - Lead 214,639
impact of environmental factors upon global
climate, as indicated by the Antarctic ozone
hole, by large temperature increases on the
Antarctic Peninsula, and by Arctic sea ice
30-Apr-13 Rainforest and savanna constitute the Y 147,857
dominant two biomes of the tropical zone.
They account for over 70% of the world's
plant species. With massive areas and with
high rates of latent and sensible heat
25-Apr-09 Just as tree rings can be used to count N 36,084
astronomical years back into the past and
ancient coral growth rings can be used to
estimate the number of days per year in the
past, layers of undisturbed sedimentary
18-May-06 The lava dome that has been growing in the Y 9,073
crater of Soufrière Hills Volcano, Montserrat
since August 2005 is now visible above the
crater rim. The dome poses increasing
hazards of collapse and explosion due its size
31-Jan-10 During the past ~100 years, mean global sea N 162,563
level has been measured to be rising at a
rate that is faster than the rate estimated for
the past few thousand years. This
accelerated rate of rise is thought to be a
9-Sep-08 Life exists wherever there is water, including N 22,832
habitats such as glaciers in the polar regions.
Dust on the surface of glaciers is heated by
the sun during the summer and melts,
forming funnel shaped features filled with
26-Nov-08 Natural archives, such as ice-cores and N 49,767
sediment records from the oceans and lakes
provide considerable evidence for the
pattern of past climatic and environmental
changes. Detailed investigations of such
5-Sep-08 The atmosphere is commonly divided into a N 125,564
number of layers or 'spheres'. Some of these
layers are characterised by an increase in
temperature with height whilst other show
an overall decrease in temperature with
31-Jan-08 The lives of many pond animals and plants N 35,658
are precarious, because ponds often dry up,
become polluted, or in various ways become
uninhabitable. Re-colonisation of ponds
often occurs through just a few colonists
23-Jan-09 This proposal is aimed at enhancing the N 250,453
international reputation of the NERC
Autosub autonomous underwater vehicle
programme and building on its science
achievements. It will sustain an international
2-Oct-09 One of the most important feedbacks in the N 164,947
natural climate system involves the emission
of gases from the ocean surface. One
important gas, dimethyl sulphide, leads to
the formation of particles in the air
30-Jun-08 Aerosols are very small liquid and solid N 189,326
particles suspended in a gaseous medium,
e.g. air. They influence the chemistry of
trace gases within the Earth's atmosphere.
This project has two parts. In the first we
13-Nov-08 Biologists use evolutionary theory as a N 159,810
means to understand and explain the natural
world. Two of the fundamental processes in
evolution are extinction where species die
out, and speciation, where new species
6-Nov-08 There is a pressing need to quantify the N 163,382
exchange of mass between the world's
oceans and polar ice caps, and this can only
be achieved by measuring how their
volumes are changing. Currently circa 50% of
31-Jan-08 The NERC DataGrid (NDG) project was Y 90,650
funded for three years from September 2002
and was built around two activities: the
development of software to support an
environmental datagrid, and deployment in
23-Mar-08 Many Institutes and university researchers N 111,163
carry out research and marine coastal and
offshore surveys and monitoring
programmes which require routine
taxonomic identification of marine plankton.
9-Aug-07 Much effort has gone into predicting how Y 27,348
climate will change in the future. Climate
change occurs if the balance between
heating the Earth (energy from the sun) and
cooling (reflection of sun-light or radiation of
9-Apr-09 Much effort has gone into predicting how Y - Lead 55,428
climate will change in the future. Climate
change occurs if the balance between
heating the Earth (energy from the sun) and
cooling (reflection of sun-light or radiation of
2-Oct-07 The NERC DataGrid (NDG) project was Y 95,315
funded for three years from September 2002
and was built around two activities: the
development of software to support an
environmental datagrid, and deployment in
30-Sep-06 We will for the first time test the feasibility N 5,109
of applying cutting edge micro-helicopter
surveillance technology to glacial research.
The surfaces of glaciers and ice sheets in the
polar regions support diverse yet poorly
30-Sep-06 The sediments recovered during this N 25,780
summer's Arctic Coring Expedition (ACEX)
give us unique insight into the nature of
Climatic and Biotic history in the Central
Arctic Ocean. This proposal is to study the
30-Sep-08 The melt of small glaciers is making a Y 61,590
substantial contribution to the rapid and
accelerating rise of global sea-level. Climate
change is predicted to have most effect on
temperature in the Arctic, making glaciers in
31-Mar-10 Greenland has a major influence on the Y - Lead 190,571
atmospheric circulation of the North Atlantic-
Western Europe region; dictating the
location and strength of mesoscale (100-km
scale) weather systems around the coastal
26-Sep-06 It is widely acknowledged that polar sea-ice N 44,280
plays a critical role in global climate change.
As such, sea-ice reconstruction should be of
paramount importance in establishing
climatic evolution of the geological past.
25-Sep-08 Both the scientific press and the broadcast Y 49,139
media have become interested in the
conjecture that increased melting of polar
ice in a globally-warming climate could cause
severe regional cooling, effectively by
11-Jan-08 The NERC DataGrid (NDG) project was Y 60,078
funded for three years from September 2002
and was built around two activities: the
development of software to support an
environmental datagrid, and deployment in
31-Dec-07 The NERC DataGrid (NDG) project was Y - Lead 475,726
funded for three years from September 2002
and was built around two activities: the
development of software to support an
environmental datagrid, and deployment in
31-May-11 To make the best use of the historical Y - Lead 235,740
research ship records as well as new
observations from autonomous ocean
profiling floats and special observing
programs such as Rapid climate change, it is
31-Jul-08 Both the scientific press and the broadcast Y 115,803
media have become interested in the
conjecture that increased melting of polar
ice in a globally-warming climate could cause
severe regional cooling, effectively by
31-Dec-08 Plankton are fundamentally important N 239,363
organisms within the marine environment,
forming the very base of almost all marine
food webs. This diverse group of organisms
are frequently referred to as being either
12-Sep-05 Research into past climate change has N 10,620
shown that the Earth experienced rapid and
recurring climate shifts during which
temperatures in the North Atlantic region
changed by up to l0ºC in a matter of
31-Jan-06 Could arctic breeding geese be speeding up N 31,097
global warming by damaging moss? Three
key features of arctic ecosystems link
together to provide the background to this
research project. 1. Important populations of
31-May-07 Human activity from land-use change and N 31,286
fossil fuel (coal, oil and gas) burning has
resulted in increasing carbon dioxide
concentrations in the Earth's atmosphere
over the last 200 years. Scientists and
31-Dec-07 The composition and softness of temperate Y 24,890
glacier ice vary spatially, but in an unknown
manner. The effects of such variations are
thereby excluded from ice flow models,
reducing their ability to predict valley glacier
29-Oct-05 N 254,424
11-Apr-08 Both the scientific press and the broadcast Y - Lead 140,125
media have become interested in the
conjecture that increased melting of polar
ice in a globally-warming climate could cause
severe regional cooling, effectively by
31-Mar-09 A free-surface, global barotropic ocean N 159,347
model has been developed and tested at
POL based on the SOC OCCAM model. This
model is capable of reproducing global
ocean tides and large-scale, deep ocean
9-Sep-06 N 249,981
8-Mar-09 Deep convection is the process by which the N 427,444
deep water of the ocean is renewed when
surface water is cooled at high latitudes and
is a key process for understanding
thermohaline circulation in the ocean. But,
3-Oct-08 The few geophysical data so far obtained N 125,210
from the northern margin of the glacier-
influenced Yermak Plateau, north of
Svalbard, indicate that a very large slope
failure has taken place. Our investigations
31-Jan-06 Evidence for modulation of climate by N 19,614
orbital forcing and atmospheric greenhouse
gas concentrations is substantial, yet our
understanding of the climatic response to
such forcing remains controversial due to
31-Jan-09 Populations at the margins of a species' Y - Lead 587,307
distribution are of interest for a variety of
reasons: to understand why a species' range
extends so far but no further, we need to
deduce what properties of the environment
31-Jan-09 Populations at the margins of a species' Y 757,404
distribution are of interest for a variety of
reasons: to understand why a species' range
extends so far but no further, we need to
deduce what properties of the environment
14-Apr-05 Small, animal-like single-celled organisms N 10,063
(microzooplankton) are an important link in
the marine food chain: they eat small phyto-
(plant) plankton and are then eaten by larger
zoo-(animal) plankton; zooplankton are
3-Mar-09 The ability to make measurements of ultra- N 297,996
trace chemical "transient tracers" in
oceanography has been of great utility in the
development of our understanding of ocean
circulation. Up to now it has not been
30-Jun-08 The sun is the fundamental source of energy N 168,458
in the Earth's climate system. However, this
source of energy varies over a number of
different timescales, including an 11-year
cycle. Variations with similar timescales have
30-Jun-09 Reliable, quantitative estimates of past N 280,857
ocean temperature are a major goal in
climate research and, given our increasing
need to understand the underlying dynamics
of the global climate system, are likely to
7-Oct-06 N 192,508
30-Sep-08 The melt of small glaciers is making a Y 64,843
substantial contribution to the rapid and
accelerating rise of global sea-level. Climate
change is predicted to have most effect on
temperature in the Arctic, making glaciers in
30-Sep-05 N 244,441
31-Aug-06 When attacked by herbivores, land plants N 101,861
can produce volatile compounds that attract
carnivorous mutualists. In this project, I will
examine whether phytoplankton use volatile
chemical cues in analogous tritrophic
31-Mar-07 N 250,995
30-Sep-08 The melt of small glaciers is making a Y - Lead 143,516
substantial contribution to the rapid and
accelerating rise of global sea-level. Climate
change is predicted to have most effect on
temperature in the Arctic, making glaciers in
31-Aug-07 The proposed research will improve our N 132,065
ability to predict future sea-level change
over the next 500 years. It relates directly to
NERC's strategic and scientific priorities, and
addresses a 'fundamental research question'
14-May-08 The chemical composition of the volatile N 181,110
elements in the deep mantle of the Earth
preserves information on the early history of
our planet. This proposal seeks funding to
perform analysis of the major and trace
31-Jul-08 Continental weathering and erosion are N 240,838
amongst the primary processes responsible
for the evolution of the landscape, exert a
major control on the transport of material
from the continents to the oceans, and on
14-Apr-05 It is known that past changes in Antarctic N 30,154
climate have been intimately linked to
variations in atmospheric CO2
concentration. In addition, rapid changes in
Greenland and Antarctic climate occurred
30-Sep-07 Periglacial solifluction (the slow downslope N 30,870
flow of saturated soils) is the main
mechanism of hillslope sediment transport
in many periglacial regions. Two distinct
styles are recognised; (a) where
31-Mar-09 This proposal is for a strategic consortium Y 188,621
grant to support the formation of a national
partnership between NERC and the
DEFRA/MoD funded Hadley Centre to
develop the capability to perform high
31-Jul-04 Supervised by Dr. Anna Ingvarsdottir, a small N 12,461
project will employ 3 student assistants for 8
weeks to make some critical measurements
on samples collected during MARPROD
Irminger Sea cruises. University of Aberdeen
31-Aug-05 For many years, ecologists have sought to N 30,976
understand the factors that enable species
to co-exist with one another in biological
diverse communities. Many theories have
been proposed to explain this species
30-Apr-05 The copepod Calanus finmarchicus is a key N 24,812
component of the North Atlantic ecosystem,
forming a vital link between primary
production and fisheries. Calanus feeds and
reproduces in the surface waters in
31-Dec-07 The composition and softness of temperate Y 34,384
glacier ice vary spatially, but in an unknown
manner. The effects of such variations are
thereby excluded from ice flow models,
reducing their ability to predict valley glacier
31-Dec-07 The composition and softness of temperate Y - Lead 86,347
glacier ice vary spatially, but in an unknown
manner. The effects of such variations are
thereby excluded from ice flow models,
reducing their ability to predict valley glacier
22-Mar-07 Localised areas (10-10 cubic m) of basal N 49,300
friction ('sticky spots') are known to be a
significant control on ice stream behaviour
and shutdown and hence, overall ice sheet
stability. Although of critical importance,
7-Mar-07 Recent NERC-funded research has revealed N 189,944
that sedimentary deposits (le dirt) can
contain DNA from plants and animals that
formerly occupied the area, up to 300,000
years ago. This finding creates a new means
30-Apr-05 The composition and softness of temperate Y 67,004
glacier ice vary spatially, but in an unknown
manner. The effects of such variations are
thereby excluded from ice flow models,
reducing their ability to predict valley glacier
31-Jan-06 Ozone (O3) is a key trace gas in the Earth's N 107,304
atmosphere, acting as an essential filter of
the sun's ultraviolet radiation and as an
agent for the natural removal of
atmospheric pollutants. Destruction of
18-Feb-08 This proposal is for a strategic consortium Y 237,165
grant to support the formation of a national
partnership between NERC and the
DEFRA/MoD funded Hadley Centre to
develop the capability to perform high
31-Dec-06 Climate change is perhaps the greatest N 196,472
environmental challenge we face. We will
need to both minimise the changes, and
adapt to the changes which are inevitable.
This research looks at one way to minimise
31-Mar-07 Open-ocean deep convection (OODC) forms Y - Lead 221,476
one end of the 'conveyor belt' of the North
Atlantic climate. We shall use the Imperial
College Ocean Model to gain a greater
understanding of the physical basis of OODC
30-Jun-09 This proposal is for a strategic consortium Y - Lead 882,823
grant to support the formation of a national
partnership between NERC and the
DEFRA/MoD funded Hadley Centre to
develop the capability to perform high
4-Nov-08 Knowledge of the history of the N 160,055
Thermohaline Circulation (THC) is crucial to
attempts to forecast it, particularly for
model validation. Cape Farewell is one of the
few locations in the North Atlantic which can
30-Nov-05 Ancient DNA will be used to reconstruct the N 29,071
evolutionary and paleoecological
relationships of the top predators of the late
Pleistocene: the giant felids (sabertooths,
lion, cheetah, jaguar, puma). Advanced
31-Oct-04 Magnetic excursions provide important N 20,416
information about the mechanisms of
magnetic field generation in the core, and
can be used to correlate climate records.
Our recent results suggest that two such
12-Jan-07 The Barents Sea is an important site for the Y 157,936
production of dense intermediate water. Up
to one half of this intermediate water flows
into the North Atlantic over the Scotland-
Greenland Ridge, constituting an important
30-Sep-06 The Barents Sea is an important site for the Y - Lead 134,747
production of dense intermediate water. Up
to one half of this intermediate water flows
into the North Atlantic over the Scotland-
Greenland Ridge, constituting an important
30-Sep-06 Salinity is a major contributor to ocean N 149,412
circulation, stability and variability. Its
structure depends on the surface freshwater
flux whose distribution is likely to change
significantly under global warming, giving
24-May-05 Through selective feeding, protists play a N 50,432
fundamental role in structuring marine
bacterial communities. Recent evidence
indicates that protists can select food based
on the cell surface properties of their prey.
29-Feb-04 Many globally significant natural hazards and N 12,185
geomorphic processes are the result of
granular or particle-laden flows. Examples
abound in our natural environment, ranging
from avalanches, debris flows, rock-falls
31-Aug-06 This proposal is for a strategic consortium Y 114,082
grant to support the formation of a national
partnership between NERC and the
DEFRA/MoD funded Hadley Centre to
develop the capability to perform high
21-Aug-08 This project will investigate the physical N 206,180
oceanographic processes occurring beneath
ice shelves, the interaction between the
polar ocean and the underside of the
shelves, and their role in determining the
3-Feb-07 This project will investigate the role that N 458,177
land ice and, in particular the Greenland ice
sheet, and sea ice play on modulating the
present day and future thermohaline
circulation in the Atlantic under a warming
31-Jan-04 We consider an idealised model of the N 24,737
winter stratospheric polar vortex and
Aleutian high, consisting of two asymmetric,
oppositely signed volumes of uniform
potential vorticity in three-dimensional
31-May-05 We propose to investigate the role of sea ice N 98,315
on seasonal to decadal variability in the
climate system through the use of the latest
datasets (spanning the years 1950-1999) and
fully coupled atmosphere-ocean-sea ice
31-Oct-06 We will investigate two aspects of the Nordic N 168,345
Seas circulation of importance to the North
Atlantic meridional overturning circulation
(MOC): (1) Sources of water in the
Greenland-Scotland overflows: recent tracer
20-Jan-06 We will investigate with unprecedented time N 102,337
resolution the sequence of events at the
start and end of two rapid climate events
observed in Greenland ice cores. Using
techniques to minimise sample volumes we
31-Dec-05 We propose to make field measurements of N 22,472
the brine volume of sea ice as it forms and
evolves in a newly formed lead. A new
instrument for this purpose will be
developed and deployed in open water
30-Jun-06 One of the most significant events in plant N 26,012
evolution was the origin of the seed.
However, it is not know from which plant
group they originated or how a single seed-
megaspore evolved from a homosporous
8-Jun-06 We will use new sampling technologies and N 263,196
techniques in an international collaboration
to collect time-series of transient tracers
penetrating the deep branch of the MOC in
the northern North Atlantic and its marginal
31-May-04 We will make Total Target Strength N 30,864
measurements of the euphausiid
Meganyctiphanes norvegica. Many
euphausiids are assessed acoustically. Echo
intensity data from acoustic surveys are
30-Apr-08 The aims of the proposal are to compare N 501,134
high-resolution isotope records from
terrestrial archives in NW Europe with model
simulations of isotopes in precipitation in
order to investigate the role of different
31-Jul-05 Overthickened mid- to lower-crust of N 26,307
continent-continent collision belts can flow
laterally under its own weight, but the
weakening mechanisms that allow flow are
largely unstudied. In the Himalaya-Tibet
30-Nov-06 The cavities beneath floating ice shelves are Y 15,304
among the least accessible places on Earth.
The development of Autosub is a unique
opportunity to undertake a coordinated
scientific effort to understand the processes
30-Sep-03 Sunlight falling onto snowpacks is known to N 24,770
photochemically produce gaseous oxides of
nitrogen. The proposer has measured UV
actinic fluxes in Arctic snowpacks and, with
simple radiation transfer code, has predicted
31-Jul-04 The dynamics of liquid aerosol droplets will N 157,697
be probed by non-intrusive optical laser
methods that can be used to determine
directly the composition and size of single
aerosol particles. The condensation and
30-Sep-05 It is now established that catalytic cycles N 74,828
involving reactive halogen species (RHS) such
as IO and BrO are responsible for
tropospheric ozone depletion events in polar
and coastal areas. Recent evidence suggests
30-Sep-05 A previous NERC funded study of DNA from N 167,025
permafrost bones revealed unexpected
patterns of localised extinctions,
replacements and genetic bottlenecks in
East Berinigian bison and bear populations
31-Aug-06 Arctic tundra landscapes exist as a mosaic of Y 102,494
vegetation (graminoid-, dwarf-shrub and
lichen-dominated) related to topography,
soil type and hydrology (wet, mesic, dry
tundra). The key driver of this fine-scale
31-Aug-06 Arctic tundra landscapes exist as a mosaic of Y - Lead 183,345
vegetation (graminoid-, dwarf-shrub and
lichen-dominated) related to topography,
soil type and hydrology (wet, mesic, dry
tundra). The key driver of this fine-scale
31-Jul-07 N 261,004
31-Jan-06 Data discovery and delivery are inherent N 825,858
components of many aspects of science.
They can be considered part of a processing
chain that starts with raw data from a
variety of sources, and ends with the
30-Nov-05 This proposal will develop a prototype ocean Y - Lead 177,889
diagnostics grid for community work with
high resolution marine data from the NERC
OCCAM model and data from the Met Office
FOAM (Forecasting Ocean-Atmosphere
31-Dec-05 Climate models predict increased N 44,900
precipitation in the arctic as global warming
progresses but are subject to error because
of incomplete representation of physical
processes and problems of downscaling. The
26-Jul-03 We propose to investigate the role of sea ice N 169,791
on seasonal to decadal variability in the
climate system through the use of the latest
datasets (spanning the years 1950-1999) and
fully coupled atmosphere-ocean-sea ice
31-Dec-05 The morphology and systematics of specific N 195,675
families within the cheilostomate Bryozoa
have been documented in some detail but
the phylogenetic relationships between
families is poorly resolved. We propose to
23-Dec-06 Decadal to millennial climate variability in N 94,537
NW Europe is tightly linked with changes in
the ocean thermohaline 'conveyor'
circulation. Deepwater exiting the Atlantic in
the South is replaced by surface returnflow.
30-Sep-05 This proposal will develop a prototype ocean Y 159,389
diagnostics grid for community work with
high resolution marine data from the NERC
OCCAM model and data from the Met Office
FOAM (Forecasting Ocean-Atmosphere
30-Sep-05 This proposal will develop a prototype ocean Y 183,971
diagnostics grid for community work with
high resolution marine data from the NERC
OCCAM model and data from the Met Office
FOAM (Forecasting Ocean-Atmosphere
31-Dec-06 We propose to use Autosub to map sea ice N 253,062
thickness and ocean structure in the
polynyas off the Filchner-Ronne and Pine
Island Glacier ice shelves in Antarctica, and,
in the Arctic, to map sea ice structure in the
14-Oct-04 Noctilucent clouds are thin layers of ice N 245,635
particles that occur around 82 km during
summer at high latitudes. They were first
reported in 1885, and have since appeared
more frequently and at lower latitudes,
11-Jun-04 Natural abundance isotope ratio (NAIR) N 51,505
signatures will be determined for
components of the zooplankton food chain
collected during Phase 2 Marine Productivity
cruises in the N.Atlantic. This will enable the
11-Sep-05 This proposal will develop a prototype ocean Y 267,968
diagnostics grid for community work with
high resolution marine data from the NERC
OCCAM model and data from the Met Office
FOAM (Forecasting Ocean-Atmosphere
8-Dec-05 The influence of the quasi biennial oscillation N 117,015
(QBO) on the interannual variability of
northern hemisphere (NH) winter polar
vortex temperatures will be studied using a
stratosphere mesosphere model and a GCM.
28-Feb-05 The AUTOSUB Under Ice thematic N 26,184
programme will use an autonomous vehicle
to carry out science missions beneath ice
cover. This proposal concerns the integration
of a digital still camera system with the
31-Dec-04 This proposal will develop a prototype ocean Y 68,784
diagnostics grid for community work with
high resolution marine data from the NERC
OCCAM model and data from the Met Office
FOAM (Forecasting Ocean-Atmosphere
31-Dec-04 The research will experimentally test the ice- N 103,858
segregation model of rock fracture in the
context of near-surface bedrock.
Experiments at the Caen Cold Laboratories
will monitor the effects of different thermal
21-Nov-04 The diversity and biogeography of benthic N 10,221
foraminifera, a dominant deep-sea taxon,
are poorly understood at both
morphological and molecular genetic levels.
To explore these issues, samples will be
4-Jan-04 We propose to use existing satellite aerosol N 44,785
extinction measurements of polar
stratospheric clouds (PSCs) to identify, for
the first time, different cloud types. This will
advance previous studies of PSCs from
31-Mar-05 This proposal aims to correlate latitudinal N 212,344
adaptation of myosin genes to the genetic
diversity of marine amphipod species
distributed from eurythermal temperate
regimes in the British Isles to cold
14-Oct-04 We will use the historical hydrographic data N 117,489
set over a million thermal profiles going back
to 1950 over the N Atlantic to investigate
variability in upper-ocean heat content.
Densities will be recovered using T/S
31-Jul-05 The iodine oxide radical IO, and the dioxide N 155,131
OIO, are present at high concentrations in
some atmospheric environments. Iodine
chemistry affects the coupling of HOx and
NOx in the atmosphere. The reaction of IO
30-Sep-05 A programme of laboratory and modelling Y - Lead 165,359
studies will be performed to investigate the
atmospheric degradation of dimethyl
sulphide (DMS) and other biogenic reduced
sulphur compounds (RSCs). These
11-Sep-04 The outstanding fossil record of planktonic N 46,725
foraminifera provides excellent proxies of
oceanography, climate change, biodiversity
and evolutionary processes. Yet, recent
molecular studies have shown that
30-Jun-05 A programme of laboratory and modelling Y 6,134
studies will be performed to investigate the
atmospheric degradation of dimethyl
sulphide (DMS) and other biogenic reduced
sulphur compounds (RSCs). These
19-Oct-04 The project aims to exploit novel satellite N 141,624
estimates of Arctic sea thickness, in addition
to existing data on ice concentration and
drift, to assess and improve the
representation of sea ice in Global
31-Jan-02 We propose the analysis of total dissolvable N 21,271
Mn in a suite of 108 recently-collected
seawater samples to detect, systematically,
for hydrothermal plumes along the
Knipovich Ridge: 74-78 degrees N,
19-Jan-04 The aim is to develop a three-dimensional, N 81,258
first-order numerical model of ice flow and
apply it to Pine Island Glacier, West
Antarctica (PIG). The two principal outcomes
of the project will be an understanding of
1-Sep-05 The project aims to determine the extent of N 246,885
genetic variation in selected species of
Antarctic lichen-forming fungi and how this
relates to modes of reproduction such as
vegetative propagation and self-fertilisation
30-Apr-03 The volume change of a number of ice caps N 35,017
and glaciers in the Svalbard archipelago will
be determined, over a five-year interval,
using airborne scanning laser altimetry. We
will deploy equipment, developed by NASA,
30-Jun-03 A numerical modelling study will be N 84,262
combined with our extensive set of
stratospheric tracer measurements to study
a number of issues relevant to ozone
depletion. We will investigate the usual
30-Jun-04 It is proposed to investigate patterns of N 248,371
muscle growth in the four morphs of Arctic
charr (Salvelinus alpinus) found in Lake
Thingvallavatn, Iceland. Hypotheses
concerning the molecular mechanisms that
30-Jun-06 A 500 GHz SIS receiver will be built, N 212,139
integrated with the THz Emission Limb
Sounder (TELIS) and deployed on the MIPAS-
B balloon gondola at ~35km altitude.
Scientific advances on RAL's 500 GHz aircraft
10-Jun-02 We propose a study of Eocene to Miocene N 6,395
benthic foraminifera from three ODP sites in
the northern Norwegian Sea (Sites 909, 913,
985) to provide a refined biostratigraphical
and taxonomical scheme that can be applied
30-Apr-03 Contrary to conventional wisdom, plants can N 33,518
take up substantial amounts of organic
nitrogen such as amino acids, potentially
eliminating the need for mineralisation. Our
team of arctic ecologists, modellers and soil
31-Aug-03 Arctic ecosystems are sensitive to climate N 35,314
change and there is already substantial
evidence for warming in many arctic regions.
We will use palaeolimnological methods to
study the effect of 20th century climate
14-Dec-03 Palaeoclimatic studies of the last glacial N 153,347
period demonstrate marked millennial-scale
climate variability in the North Atlantic
region. We intend to produce century-scale
resolution records of surface ocean
29-Feb-04 Ichthyostega was the first Devonian tetrapod Y 53,572
discovered, yet it remains the most
misunderstood, its potential importance
unexplored. This project will reconstruct its
anatomy using new material to provide a
18-Feb-02 Funding is requested to provide a PDRA for N 36,645
one year to develop and test a prototype,
compact, fast-response sensor for
tropospheric IO and NO2 at concentrations
as low as 2 and 20 ppt respectively with only
31-Jan-02 We aim to use the results of our geophysical N 35,404
and geological investigations (side-scan
sonar, seismics and cores) and numerical
modelling of the processes and patterns of
glacier-influenced sediments on the
28-Feb-05 This project will investigate the impact of N 151,193
salinity anomalies in the Nordic and Arctic
Seas on climate. It will determine whether
they result from feedbacks in the coupled
ocean, atmosphere and/or sea-ice systems,
7-Jul-01 Researchers at NASA, while examining N 22,530
SeaWiFS satellite pictures of the Bering Sea
this winter, noticed unexpected, large, high-
reflectance features (see image in case for
support). The cause of this phenomenon is
30-Nov-03 Ichthyostega was the first Devonian tetrapod Y - Lead 105,145
discovered, yet it remains the most
misunderstood, its potential importance
unexplored. This project will reconstruct its
anatomy using new material to provide a
30-Nov-03 This project will quantify annual nitrogen N 291,923
fluxes, following snow melt, in a pristine high
Arctic ecosystem on Svalbard (78?N), we
shall utilise the complementary approaches
of 15N-labelling the melting snowpack and
30-Nov-06 Antarctic marine invertebrates live at one N 217,393
extreme of conditions available in the
world's oceans. Their environment is one of
low, but extremely stable temperature, and
they can live only within narrow
31-Jan-02 The accumulation and depletion of snow N 34,900
cover have been indentified as of critical
importance to the operation of atmospheric
models. This Proposal seeks to i) improve
the understanding of surface processes and
30-Sep-01 Ediacaran fossils represent the oldest known N 26,103
animal-like organisms, and their best
preservation, largest diversity and widest
stratigraphic range occur in the White Sea
area, NW Russia. We propose to document
30-Sep-02 The aim of the project is to reconstruct N 25,214
changes in ice-cover duration in Europe
based on changes in diatom assemblage in
high mountain lakes. Physically based
mathematical models of the effects of
31-Aug-03 Three problems will be addressed. Deep N 127,042
water production within polynyas is not
resolved in global OGCMs. By developing a
polynya flux model coupled to an ocean and
atmosphere model, a parameterisation of
20-Aug-02 Our aim is to build on previous NERC funded N 98,553
research to provide three deliverables within
a programme to produce the first ever self-
consistent atmospheric aerosol and
photochemistry study based on the "state of
31-Jan-04 Recent evidence has shown that semi- N 143,377
volatile , persistent organic pollutants (POPs)
are effectively scavenged by snow. In high
latitudes where snow plays a major part in
the hydrological cycle, it is a significant
31-Dec-03 Controversy over how early Archean crust N 49,345
was generated with two models being
proposed. One proposes gradual
accumualtion over c300 Ma whilst the other
argues formation in one super-event. Within
6-Sep-02 Recent work in Greenland and Antarctica has N 117,300
provided compelling evidence that the upper
layers of snowpack are a significant source
of NOx (and probably other important
species) to the polar lower troposphere, and
31-Oct-01 Over the past 3 decades much effort has N 58,813
been expended on measuring the fecundity,
growth and production of copepods. This has
led to attempts to try and predict these
rates, and to understand which factors are of
31-Oct-01 The persistence of different species of N 76,009
zooplankton within a region is dependent on
it's vertical migration behaviour. Vertical
migration behaviour is influenced by many
factors including food availability, predation
30-Apr-03 Development of a turbulent discharge flow N 83,803
(DF) reactor for kinetic and mechanistic
studies of key gas phase radical reactions as
f(T, p). Use of chemical ionisation mass
spectrometry (CIMS) detection incorporating
30-Jun-03 This study would investigate the effects of N 200,469
simulated pollutant nitrogen on species
diversity and function of communities of
decomposer fungi from a high arctic polar
semi-desert ecosystem. The direct effects on
28-Feb-03 Centrifuge scaling laws allow similitude N 57,636
between scaled models and their prototypes
in terms of self weight stresses, and, since
both seepage force similarity and conductive
heat transfer scale as 1/N2, where N is the
22-Feb-01 A series of gas tropospheric measurements N 15,166
are proposed within the Arctic region as a
component of the ARCICE Thematic
Programme 1999 Arctic cruise. This project
aims to produce an accurate estimate of the
31-Jul-01 This project aims to elucidate the processes N 31,961
of nutrient acquisition and transport by
meltwaters in transit to an arctic fjord. A
field study of the nutrient content of two
winter snowpacks and of the concentrations
30-Apr-03 Mat-forming lichens offer promise as N 131,602
indicators of N deposition in the remote
north since their N-status is correlated with
atmospheric N income. This view is
compromised by reports of low thallus *15N
15-Apr-01 This project will determine the likely N 88,630
evolution of the Antarctic ice sheet (AIS)
using a state-of-the-art numerical model.
This will be achieved by first simulating the
present-day state of the AIS. The stability of
4-Nov-01 The NASA measurement campaign SOLVE is N 88,310
designed to examine the processes that
control lower stratospheric and upper
tropospheric ozone levels at mid- to high-
latitudes. We propose to contribute to the
31-Oct-02 The contribution of Svalbard glaciers to sea Y 32,713
level rise has been estimated to be larger
than that of any other Arctic region outside
Greenland. The accuracy of this estimate,
based on extrapolation of measurements
31-Oct-02 N 1,987,927
17-Oct-00 The basic hypothesis is that respiratory N 35,087
metabolism, including the engagement of
the alternative oxidase is crucial to plant
adaptation to Arctic environments. The
proposal is to develop and validate a field
30-Apr-03 An improved understanding of the glacier N 53,269
hydrology and ice dynamics of high Arctic
glaciers is critical if the potential importance
of the contribution of runoff from these
glaciers in response to climate change is to
19-Oct-02 Laboratory studies of the gas phase kinetics N 114,837
and mechanisms of key organic peroxy
radical reactions under conditions relevant
to the UTLS. Theoretical calculations of the
energetics and rate coefficients for these
31-Dec-01 This proposal addresses the geometry and N 153,394
flow dynamics of three large ice caps in the
Canadian arctic islands, with implications for
glacier mass balance and the rate of sea-
level change in a warming world. The work
30-Jun-03 A survey of the ice caps and glaciers of the N 119,376
Russian and Canadian High Arctic glaciers
and ice caps, and the North West Greenland
ice sheet, will be performed using
interferometry. Complex radar images from
31-Jul-02 Arctic and Antarctic microbial plankton N 144,311
communities appear to follow very different
winter survival strategies, probably related
to water column light, climate and other
physical and chemical factors. These
31-Oct-01 To develop a field portable sample N 51,028
enrichment device to interface with and to
extend existing field GCMS capabilities to
determine the long lived, highly volatile
fluorocarbons in the atmosphere. To carry
30-Jun-03 In this project we intend to identify and N 146,925
quantify sources of methane in the
continents bordering the Atlantic by
measuring CH4 and CO concentrations and
isotopes in air sampled at Atlantic
31-May-02 Y 92,937
30-Nov-01 Fluxes of heat, moisture, radiation and Y - Lead 80,179
momentum vary considerably between
ice/atmosphere interfaces. The intermingling
of ice and ocean surfaces in the marginal ice
zone causes highly complex behaviour of
31-Jul-02 This project addresses a key aim of the N 85,836
ARCICE programme - the dynamics of Arctic
continental margins since the last glacial
maximum (LGM). The work will involve two
cruises in Disko Bugt, West Greenland,
31-Mar-01 We will use a sophisticated 3D chemical N 77,572
transport model, in conjunction with a wide
range of observations to be obtained as part
of the EU THESEO programme in 1998/99, to
study the cause of the downward trend in
30-Sep-01 N 125,579
31-Mar-02 The purpose of the proposed project is to N 123,328
determine the hemispheric offsets in 14C for
the period ad 1000 to ad 1710 using decadal
samples of tree-ring-dated wood from New
Zealand and the British Isles. Doing so will
31-Jul-02 The understanding of the inter-relationship N 129,004
between stratospheric ozone change and
stratospheric temperature change is of
essential importance in establishing links
between ozone and climate change. We
23-Jul-03 We propose a study of the effect of sea ice Y - Lead 137,603
on oceanic vertical circulation, meaning the
local vertical exchange of water properties in
the Greenland Sea by convection, both to
greater and lesser depths; the transfer of
21-Mar-02 We will investigate the origin of ice-melt N 142,967
input to, and inter-mixing with , the water
masses around the Greenland Sea. The role
of ice and freshwater inputs in both limiting
and promoting deep convection, and the
14-Mar-02 Preliminary studies have revealed that arctic N 158,473
permafrost deposits of late Pleistocene
mammalian bones contain considerable
amounts of preserved DNA, providing an
opportunity to examine the genetic
14-Jun-02 The response of ice sheets and glaciers to Y - Lead 46,333
climatic forcing ( and thus any resultant sea
level change ) depends not only on mass
balance changes , but more importantly on
the nature of the underlying substratum (
18-Aug-01 Y 39,194
31-Jul-01 Y 35,237
31-Mar-02 We propose to construct a new noble gas N 69,640
static vacuum isotope ratio-mass
spectrometer that is optimised for 3he/4he
isotope ratio measurements and noble gas
concentration measurements. Initial
30-Sep-02 The aims of the project are to develop a UK N 116,544
leading edge high resolution ocean-sea ice
model covering the Arctic and Nordic seas
and to use it, together with the results of
earlier runs of the OCCAM model , to: (a)
17-Jul-02 The contribution of Svalbard glaciers to sea Y 18,848
level rise has been estimated to be larger
than that of any other Arctic region outside
Greenland. The accuracy of this estimate,
based on extrapolation of measurements
14-Jan-02 Variations in ice-ocean-climate interactions Y - Lead 215,030
on the polar North Atlantic margins have
produced a distinctive record, including huge
submarine fans, slides and channel systems,
and deep-ocean sediments which indicate
31-Dec-01 Y 180,050
31-May-02 The expected future global warming will N 159,369
increase the significance of melting in the
mass balance of all arctic ice masses. It is
typically confined to a narrow band around
the perimeter of the ice sheet. Thus
30-Jun-02 The contribution of Svalbard glaciers to sea Y 19,372
level rise has been estimated to be larger
than that of any other Arctic region outside
Greenland. The accuracy of this estimate,
based on extrapolation of measurements
30-Jun-02 The contribution of Svalbard glaciers to sea Y - Lead 54,648
level rise has been estimated to be larger
than that of any other Arctic region outside
Greenland. The accuracy of this estimate,
based on extrapolation of measurements
31-Jul-02 There is little hydrochemical data in the N 187,927
literature to assess the chemical weathering
of granite and continental shield by larger ice
masses, despite these being the lithologies
that underlay large areas of the Laurentide
30-Jun-02 Recent literature has identified the pro- N 68,488
glacial zone as a region which may support
globally significant rates of chemical
weathering, particularly during deglaciation.
However, this remains conjecture until field
31-Oct-02 The project aims to exploit novel and unique N 124,833
techniques to extract ocean variability, tides
and sea ice freeboard from spaceborne
altimeter measurements over the Arctic
Ocean. High precision measurements of
29-Sep-01 N 88,254
30-Sep-02 HIRDLS is an infrared limb sounder to N 2,185,085
measure stratospheric temperature and
constituents from the NASA EOS Chem-1
satellite to be launched in 2002. The
measurements will be used to advance our
31-Aug-01 Cretaceous/palaeogene diatomites have N 17,260
been routinely interpreted as the product of
upwelling yet this is at variance with
concepts of sluggish circulation in salinity-
stratified oceans at that time. On the basis of
30-Sep-01 From research undertaken at the Culture N 24,203
Collection of Algae and Protozoa (CCAP), and
elsewhere, the role of freeze-induced
damage appears to be a major factor causing
viability loss in organisms subjected to low
31-Aug-01 The study aims to build theoretical models N 10,176
of fully developed convection and
solidification in sea ice. Concurrently, we will
determine the associated fluxes of heat and
mass and investigate the effects of the
31-Aug-01 N 91,773
31-Mar-01 N 664,439
30-Sep-01 N 2,373,823
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