offshore
Shared by: niusheng11
-
Stats
- views:
- 7
- posted:
- 12/4/2011
- language:
- English
- pages:
- 4
Document Sample


Intro
The offshore boat work was carried out to investigate the chemical, physical and biological processes
occurring spatially within the water column from the mouth of the Fowey estuary along the south
coast of Cornwall to the mouth of the Fal estuary. Coastal regions are diverse areas with complex
habitats and environments which are also influenced by the proximity to human populations along
the coastline (Jahnke et al., 2008). The aim of the offshore investigation is to use a combination of
instruments to observe the vertical mixing processes affecting the planktonic communities occurring
within the water column. From previous studies it is known that there is summer thermal
stratification in the English Channel (Smyth et al., 2010). Looking at the stratification of the water
column gives the physical properties, which can be linked to the distribution of phytoplankton which
are expected to be in high abundance around the thermocline (Smyth et al., 2010) as at this depth
there is a compromise between high solar radiation and the availability of nutrients which decrease
in the upper water column over the summer months due to the thermal stratification and being
depleted during the spring phytoplankton bloom (Obata et al., 1996). The zooplankton populations
are expected to occur in the highest abundance below the phytoplankton, avoiding prey from above
as well as feeding on the phytoplankton. Dissolved oxygen gives an indication of the balance
between autotrophy and heterotrophy whilst phosphate and silicon were also collected to observe
the vertical mixing of the chemical processes occurring along the Cornwall coastine.
Method
The investigation took place from RV Callista on 05 July 2011. Cast off from Prince of Wales Pier was
at 0735 GMT and the ADCP was started at 0804 GMT. There was then travel time of approximately 2
hours to the first station which was along the coast to the east of Falmouth. The weather began as
overcast with occasional drizzle and improved to sunshine with intermittent cloud cover after 1200
GMT. The wind in the morning was 12-15 mph with gusts up to 22mph dropping to 10-12 mph with
gusts of 15mph in the afternoon.
The ADCP was continually run between stations and at stations throughout the investigation. Five
CTD stations were taken between Fowey and Falmouth. Zooplankton was collected at station 1, 2, 3
and 5 using a zooplankton net and a Bongo net at station 3. Phytoplankton, dissolved oxygen,
phosphate and chlorophyll were collected by a Niskin bottle at each station.
Station Location (Lat and Long) Time (GMT) Depth (m)
1 50° 17.700 N 1040 23.3
004° 37.639 W 0.0
2 50° 19.172 N 1050 15.0
004° 38.593 W 0.0
3 50° 15.520 N 1204 28.0
004° 41.775 W 0.0
4 50° 13.571 N 1337 19.0
004° 47.002 W 0.0
5 50° 13.016 N 1341 20.0
004° 47.124 W 0.0
6 50° 08.705 N 1549 23.0
005° 01.450 W 0.0
References
Smyth, T.J., Fishwick, J.R., Al-Moosawi, L., Cummings, D.G., Harris, C., Kitidis, V., Rees, A.,
Martinez-Vincente, V. and Woodward, E.M.S. 2010, ‘A broad spatio-temporal view of the
Western English Channel observatory’, Journal of Plankton Research, 32, 585-601
Obata, A., Ishizaka, J. and Endoh, M. 1996, ‘Global veification of critical depth theory for
phytoplankton bloom with climatological in situ temperature and satellite ocean color data’,
Journal of Geophysical Research, 101, 20657-20667.
Jahnke, R.A., Roman, M.R. and Brink, K.H. 2008, ‘Coastal Ocean Processes Program’,
Oceanography, 21, 18-21.
Time Depth
GMT LAT N LONG W (m)
07:35 cast off
08:04 start ADCP 000 50 08.164 005 00.104
10:40 station 1 50 17.700 004 37.639 23.3
10:40 0
10:50 end ADCP 001 50 17.871 004 37.643
10:50 start ADCP 002 50 17.871 004 37.643
10:50 station 2 50 19.172 004 38.593 15
10:50 0
end 002 start
11:04 003 50 19.172 004 38.593
end 003 start
11:34 004 50 19.092 004 38.730
12:04 station 3 50 15.520 004 41.775 28
12:04 start stop 0
12:04 bongo 31100 31715
12:04 (100um) 1251 1257
end 005 start
13:08 006 50 14.827 004 42.046
end 006 start
13:32 007 50 13.571 004 47.002
13:37 Station 4 50 13.571 004 47.002 19
13:41 Station 5 50 13.016 004 47.124 20
end 007 start
13:41 008 50 13.016 004 47.124 0
end 008 start
13:56 009 50 12.859 004 49.054
end 009 start
14:34 010 50 12.423 004 48.968
end 010 start
15:37 011 50 08.705 005 01.450
15:49 station 6 50 08.705 005 01.450 23
15:49 0
16:15 end 11 50 08.998 005 01.715
http://www.tos.org/oceanography/issues/issue_archive/issue_pdfs/21_4/21.4_jahnke_intro.pdf
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 101, NO. C9, PAGES 20,657-20,667, SEPTEMBER 15, 1996
Global verification of critical depth theory for phytoplankton
bloom with climatological in situ temperature
and satellite ocean color data
Atsushi Obata
JOURNAL OF PLANKTON RESEARCH j VOLUME 32 j NUMBER 5 j PAGES 585–601 j 2010
A broad spatio-temporal view of the
Western English Channel observatory
TIMOTHY J. SMYTH*, JAMES R. FISHWICK, LISA AL-MOOSAWI, DENISE G. CUMMINGS, CAROLYN HARRIS,
VASILLIS KITIDIS, ANDREW REES, VICTOR MARTINEZ-VICENTE AND ERNEST M. S. WOODWARD
Related docs
Other docs by niusheng11
Get documents about "