Meeting the Climate Change Challenge
Document Sample


Meeting the Climate Change Challenge:
Avoiding the Unmanageable, Managing the Unavoidable
John P. Holdren
Assistant to the President for Science and Technology
and Director, Office of Science and Technology Policy
Executive Office of the President of the United States
Keynote Address for the
2009 World Maritime Day US Event
New York, NY • 16 October 2009
Coverage of these remarks
• Essence of our energy-climate predicament
• Energy: Where we are, how we got here, where
we’re headed
• Climate change: What’s already happening,
what lies ahead absent a course change
• Technical options
• Policy goals, tools, and outlook
• A bit about climate change & national security
The essence of our energy-climate
predicament
• Without energy there is no economy.
• Without climate there is no environment.
• Without economy and environment there is no
material well-being, no civil society, no national
or personal security.
Alas, the world is getting most of the energy its
economies need in ways that are wrecking the
climate its environment needs.
Energy -- how we got here: Growth of world
population & prosperity 1850-2000 20-fold
energy growth, nearly all of it from fossil fuels
Growth rate 1850-1950 was 1.45%/yr, driven mainly by coal.
From 1950-2000 it was 3.15%/yr, driven mainly by oil & natural gas.
The energy-CO2 picture in 2008
population ppp-GDP energy fossil E fossil CO2
(millions) (trillion $) (EJ) (percent) (MtC)
World 6692 69.7 545 82% 8390
China 1326 7.9 99 85% 1910
USA 304 14.2 105 86% 1670
Russia 142 2.3 30 91% 440
India 1140 3.4 29 64% 390
Brazil 192 2.0 10 58% 100
But Brazil adds 200-400 MtC/yr from deforestation.
Where we’re headed under BAU: by 2030, energy
+60%, electricity +75%, continued fossil dominance
Primary energy
WEO 2007
What’s wrong with this picture?
• Multiple reasons for changing course include
– high US oil imports & increasing international
competition for oil involving China, USA, & others
– conventional air pollution, water pollution, and
ecosystem impacts from fossil-fuel harvesting & use
• But most compelling reason (which also requires
the fastest, biggest course change) is dominant
role of fossil-fuels in global climate-disruption
– energy accounts for ~70% of global emissions of the
heat-trapping gases & particles wrecking the climate
(the other 30% are from deforestation, agriculture,
waste management, cement production)
Climate change: what’s already happening
• Climate change is occurring faster than
previously predicted
– emissions & concentrations rising at rates at or above
those of earlier IPCC “high” scenarios
– temperatures are increasing, glaciers retreating, sea
ice shrinking, permafrost thawing, Antarctic &
Greenland ice sheets slipping, sea level rising
• Significant harm to human well-being is already
occurring
– increases in floods, droughts, wildfires, heat waves,
pest outbreaks; poleward spread of tropical diseases
– avoiding “dangerous” human interference is no longer
possible: we’re experiencing “dangerous” now
Global average T as recorded by thermometers
NASA Goddard Institute
We know what’s
causing it.
Top panel shows best
estimates of human
& natural forcings
1880-2005.
Bottom panel shows
that state-of-the-art
climate model, when
fed these forcings,
reproduces almost
perfectly the last
125 years of
observed
temperatures.
Source: Hansen et al.,
Science 308, 1431, 2005.
Glaciers are retreating
Sea ice is shrinking
...and thinning: sea ice age at Sept minimum
Greenland and Antarctic ice sheets are losing mass
Harm is already occurring: floods & droughts
Weakening East-Asia monsoon – attributed to global climate
change -- has meant less moisture flow South to North,
producing increased flooding in South, drought in North
Qi Ye, Tsinghua University, May 2006
Harm is already occurring: wildfires
Wildfires in the Western USA have increased 4-fold in the last 30 years.
Similar trends are evident in other fire-prone regions.
Western US area burned
Source: Westerling et al., SCIENCE, 2006
Harm is already occurring
In fact worldwide we’re seeing increases in
• floods
• wildfires
• droughts
• heat waves
• pest outbreaks
• coral bleaching events
• power of typhoons & hurricanes
• geographic range of tropical pathogens
Climate change: Where are we headed?
Last time T was 2ºC
above 1900 level was
130,000 yr BP, with
sea level 4-6 m higher
than today.
Last time T was 3ºC
above 1900 level was
~30 million yr BP, with
sea level 20-30 m
EU target ∆T ≤ 2ºC higher than today.
Note: Shaded bands
denote 1 standard
deviation from mean
in ensembles of model
runs
IPCC 2007
Where we’re headed: Heat waves
Extreme heat waves in Europe, already 2X more frequent because of
global heating, will be “normal” in mid-range scenario by 2050
Black lines are
observed
temps,
smoothed &
unsmoothed;
red, blue, &
green lines are
Hadley Centre
simulations w
natural &
anthropogenic
forcing; yellow
is natural only.
Asterisk and
inset show 2003
heat wave that
killed 35,000.
Stott et al., Nature 432: 610-613 (2004)
Where we’re headed: Agriculture in the tropics
Crop yields in tropics start dropping at local ∆T ≥ 1-
1.5°C
Easterling and Apps, 2005
Where we’re headed: droughts
Drought projections for IPCC‘s A1B scenario
Percentage change in average duration of longest dry period, 30-year
average for 2071-2100 compared to that for 1961-1990.
Where we’re headed: Oceans acidifying as well as
warming
pH history and “business as usual” projection
Red line is global annual
average; blue lines show
ocean-to-ocean and
seasonal variation.
Surface ocean pH has already
fallen by 0.1 pH unit. Projected
additional changes are likely to
have large impacts on corals and
other ocean organisms that make
skeletons/ shells from calcium
carbonate.
What might happen: Tipping points
• If Arctic sea ice disappears entirely and doesn’t
re-form, climate of N hemisphere would change
drastically.
• Tundra & permafrost are warming & thawing, with
potential for CO2 and methane outpouring that
would accelerate climate disruption overall.
• Rapid ice-sheet disintegration (1-2 m per century
sea-level rise) possible for ∆Tavg ≥ 1.5ºC.
Sea level could rise 1-2 meters by 2100,
3-12 m in the next few hundred years,
up to 70 m eventually.
What would 1-70 m of sea-
level rise do to your region?
Courtesy Jeffrey Bielicki, Kennedy School of Government
What are our options?
There are only three:
• Mitigation, meaning measures to reduce the pace
& magnitude of the changes in global climate being
caused by human activities.
• Adaptation, meaning measures to reduce the
adverse impacts on human well-being resulting
from the changes in climate that do occur.
• Suffering the adverse impacts that are not avoided
by either mitigation or adaptation.
Mitigation possibilities
CERTAINLY
• Reduce emissions of greenhouse gases & soot
from the energy sector
• Reduce deforestation; increase reforestation &
afforestation
• Modify agricultural practices to reduce emissions
of greenhouse gases & build up soil carbon
POSSIBLY
• “Geo-engineering” to create cooling effects
offsetting greenhouse heating (white roofs...)
• “Scrub” greenhouse gases from the atmosphere
technologically
Adaptation possibilities include…
• Changing cropping patterns
• Developing heat-, drought-, and salt-resistant
crop varieties
• Strengthening public-health & environmental-
engineering defenses against tropical diseases
• Building new water projects for flood control &
drought management
• Building dikes and storm-surge barriers against
sea-level rise
• Avoiding further development on flood plains &
near sea level
Some are “win-win”: They’d make sense in any case.
Mitigation & adaptation are both essential
• No feasible amount of mitigation can stop climate
change in its tracks.
• Adaptation efforts are already taking place and
must be expanded.
• But adaptation becomes costlier & less effective
as the magnitude of climate changes grows.
• We need enough mitigation to avoid the
unmanageable, enough adaptation to manage
the unavoidable.
How much mitigation is enough?
• 550 ppmv CO2-e (50% chance of ∆Tavg < 3 C)
looks unlikely to avoid unmanageable change
• 450 ppmv CO2-e (50% chance of ∆Tavg < 2 C)
would be more prudent (but still no guarantee)
• Achieving 450 ppmv requires that...
– global emissions level off by ~2020 and
decline thereafter to ~50% below 2000
emissions by 2050.
– emissions in USA & other industrial countries
level off by 2015 and decline thereafter to
~80% below 2000 emissions by 2050.
The essential steps in climate policy
• Remove barriers to “win-win” solutions
– lack of information, perverse subsidies & regulations
• Put a price on GHG emissions
– tax or cap-and-trade, to make costlier solutions pay off
• Increase investments in energy-technology
research, development, demonstration (ERD&D)
– 2-4x increase in public direct expenditures + tax
incentives for increased private effort
• Expand partnerships (public-private, internat’l) for
deploying advanced energy technologies
– include internat’l fund for low- and no-carbon options
• Achieve a new global agreement for mitigation
and adaptation in the post-2012 period
– aimed at declining global emissions by 2020 &
including compensation for avoided deforestation
Congress and Copenhagen
• What’s needed from Congress is legislation that
will get the USA on a path to level off emissions
by 2015 and decline steadily thereafter.
• What’s needed at the Copenhagen Conference
of the Parties to the 1992 UN Framework
Convention on Climate Change is a global
agreement under which developing countries
agree to join industrialized nations on declining
emissions trajectories no later than 2025.
There’s little chance the latter will happen
unless the former does.
The Obama administration’s strategy
• Promote recognition that this isn’t “climate
change policy versus the economy” but “climate
change policy for the economy”.
– costs of action, for the USA and the world, will be far
smaller than costs of inaction
– we can reduce costly and risky oil imports and
dangerous air pollution with the same measures we
employ to reduce climate-disrupting emissions
– the surge of innovation we need in clean-energy
technologies and energy efficiency will create new
businesses & new jobs and help drive economic
recovery, growth, and global competitiveness.
Obama administration strategy (continued)
• Work with Congress to get comprehensive energy-climate
legislation that will put the USA on the needed emissions
trajectory with minimum economic & social cost &
maximum co-benefits.
Waxman-Markey isn’t perfect, but it’s a good start and
possibly can be improved in Senate and Conference.
• Work with other major emitting countries – industrialized &
developing – to build technology cooperation and
individual & joint climate policies consistent with “avoiding
the unmanageable”
• Develop adaptation strategies and capacities domestically
and internationally to “manage the unavoidable”.
Can we get it done? Polls say “Yes, we can.”
http://www.worldpublicopinion.org/pipa/images/dec07/CCdigest/CCgraph1.htm
Climate connections to national security
Climate change itself can have impacts on…
• types of missions security forces must perform
• effectiveness of troops & equipment in combat
• international tensions increasing chance of conflict
Remedies for climate change may increase…
• tensions/vulnerabilities from energy dependencies
• access of states & terrorists to nuclear weapons
• international cooperation (reducing tensions)
Both impacts and remedies could reduce…
• funding for forces and readiness
Climate-security connections (continued)
Impacts of climate change on types of missions
• floods, droughts, wildfires, powerful storms, pest
outbreaks increased “civil defense” demands
• ice-free Arctic ship traffic, resource-harvesting
operations increased patrol requirements
Impacts of climate change on effectiveness
• complication of combat operations by increased
heat, dust, mud, storms, flooding…
• impacts on troop health by worsened disease
environment (malaria, dengue…)
• impacts on viability, effectiveness of bases
Climate-security connections (continued)
Impacts of climate change on tensions
• water shortages in international river basins
increased disputes & tensions
• ice-free Arctic tensions over ownership of and
access to undersea resources there
• suffering civil disorder, government instability
oppression, external conflict as a distraction
• suffering large flows of environmental refugees
civil disorder, reaction-intervention
• disputes & tensions over responsibility and
compensation for climate-change damages
Related docs
Get documents about "