the arctic region in a climate change worldthe arctic region in a climate change world the...
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The Arctic Region in a Climate Change World
The Scientific Foundations for Policy
Pathways forPathways for Copenhagen and
BeyondBeyond
Dr. Robert W. Corell, Chair of the Climate Action Initiative, an International Partnership
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“The stakes are high. Climate change has profound implications for virtually allhas profound implications for virtually all aspects of human well being, from jobs and health to food security and peaceand health to food security and peace
within and among nations. Yet too often climate change is seen as anclimate change is seen as an
environmental problem when it should be part of the broader development andpart of the broader development and
economic agenda. Until we acknowledge the all-encompassing nature of the threatthe all encompassing nature of the threat,
our response will fall short.”Kofi Anan. Former Secretary General of the United Nations
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621
CO2
C t tiLet’s look at the Earth’s climate d ring the time that h manit as Concentrations over
the past 400,000 years, with current
during the time that humanity, as we know it, established itself.
CO Levels Now at ~ 385 ppmv
ylevels of CO2 higher than they have been
in 800 000 yearsCO2 Levels Now at ~ 385 ppmv in 800,000 years.
CO2 Pre-Industrial Levels where at ~ 280 to 300where at 280 to 300
ppmv
Let’s look at thisLet s look at this scale of time, the past 10,000 years or so.
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Ice Core data A shopping list
Tiny Hollow Spheres with Captured Samples
pp g
• The ice: 18O , 17O , 16O, 1H og 2DC• Continental dust, volcanic ash, micro metheorites and biological materialI Cl NO SO 2 F H N K• Ions: Cl-, NO3
-, SO42-, F-, H+, Na+, K+,
NH4+, Mg2+, Ca2+
• Gas in air bubbles: CO2, CH4, O2, N2, SF
Cross-Section of an Ice Core SF6.
• Radioactive isotopes: 10Be, 36Cl, 210Pb, 32Si, 14C, 137Cs, 90Sr.
Ice Core
• DNA• Ice Properties • Bore hole logging: temperature, gg g p ,
geometryNatural ice through polarized light(sample size : 4 x 10 cm)
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One DegreeDegree Matters
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We face an incredible challenge: Emissions now exceed theWe face an incredible challenge: Emissions now exceed the IPCC Worst-case Scenario.
mis
sion
s yr
) (IPCC Worst-Case)
sil F
uel E
m(G
tC/y (IPCC Worst Case)
Foss
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Year 2008Atmospheric CO2 Concentration
At thisYear 2008Atmospheric CO2
Concentration:
At this accelerating
rate we will be at 500 ppm byConcentration:
387 ppm~ 40% above pre industrial
at 500 ppm by 2050
~ 40% above pre-industrialGrowth in Atmospheric CO2 Concentrations/Year
1970 - 1979: 1.3 ppm/yearpp y1980 - 1989: 1.6 ppm/year1990 - 1999: 1.5 ppm/year er
atin
ger
atin
g
pp y2000 - 2007: 2.0 ppm/year
2007: 2.2 ppm/year Acc
ele
Acc
ele
Data Source: Pieter Tans and Thomas Conway, NOAA/ESRL
pp y2008: 2.3.ppm/year
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Global Carbon Project October 2008 ReportNewDataNewData
• Since 2000, CO2 emissions derived from human sources have been growing x4 faster than in the g g1990s and are now above the worst case emission scenario of the Intergovernmental Panel on Climate Change.
• Despite 15 years of intense international climate negotiations, concentrations of CO2 in the atmospheric have been growing 33% faster during th l t 8 th i th 1990the last 8 years than in the 1990s.
• These drivers of climate change are accelerating.
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~ 20%Fate of Anthropogenic CO2 Emissions (2000-2007)
20%Atmosphere
46%4.2 Pg Carbon/yr4.2 Pg Carbon/yr
~ 46%
(1 5 Pg Carbon /yr)
+~ 80%Land
~ 29%
(1.5 Pg Carbon /yr)
80%2.6 Carbon Pg/yr2.6 Carbon Pg/yr D
own by 5
Dow
n by 5
Oceans~ 26%
2 3 Carbon Pg/yr2 3 Carbon Pg/yr(7.5 Pg Carbon /yr)
5%5%
Canadell et al. 2007, PNAS (updated)
2.3 Carbon Pg/yr2.3 Carbon Pg/yr( 5 g Ca bo /y )
Down ~ 5%
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Let’s look at the role the oceans play in the dynamics of climate change.
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Why are the oceans Important?Why are the oceans Important?
Because that is where the heat goes !Because, that is where the heat goes !
Data from Levitus et al, Science, 2001
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Warming of the World’s Oceans(An Analysis of the past 40 Years)
No Anthropogenic Forcing (Blue)
With Anthropogenic
Observational Data (Red Dots)
Forcing (Green)
Source: T.P. Barnett, et al 2005
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Does this Melting of Sea Ice have other Effects, such as an Impacts on Oceanic Circulation?
Critical RegionCritical Region
as an Impacts on Oceanic Circulation?
Critical RegionCritical Region
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Changes in Oceanic Temperatures of Importance.Changes in Oceanic Temperatures of Importance.
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Conveyor OFF
• Strong cooling in North Atlantic
• Strong cooling in North Atlanticin North Atlantic
• Warming everywhere else
in North Atlantic
• Warming everywhere else
• No net global change
• No net global change
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Marine Species Impacted by Ocean Acidification
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Ocean AcidificationWhat are the prospects for the coming decades?
Avoiding Dangerous Climate Change (Turley et al 2006)
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QuickTime™ and aH.264 decompressor
are needed to see this picture.
The Arctic is now experiencing some of the rapid and severe climate change on Earth!
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The Arctic region is facing dramatic hchanges
• Substantial Changes in Climate d th
• Substantial Changes in Climate d thand weather
• Rapid cultural and social changeand weather
• Rapid cultural and social change• Globalization such as mixed
economies and technological • Globalization such as mixed
economies and technological gchanges
• High Concentrations of
gchanges
• High Concentrations ofHigh Concentrations of Contaminants such as PCBs and mercury
High Concentrations of Contaminants such as PCBs and mercurymercury
• Ozone depletion that leads to UV i
mercury• Ozone depletion that leads to UV
i
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September 10 - 14, 2009September 10 - 14, 2009p ,p ,
140 Years = An Increase of 1.25 OC or 2.25 OF
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Recent Findings:ACIA Model Projections j
in 2004
4 1 Million Square Kilometers on4.1 Million Square Kilometers on September 15, 2008
Actual Sea Ice Extent 2007
and 2008and 2008
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Arctic Sea Ice Conditions on September 15th 20082008
Greenland
R iRussia
AlaskaAlaska
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Projections of Sea Ice Extent for Mid-SeptemberProjections of Sea Ice Extent for Mid-SeptemberThese open waters dramatically change the balance of reflected radiation from These open waters dramatically change the balance of reflected radiation from
Recent Model Runs Suggest this by 2030 -
plus or minus a decade
about 85% reflected to about 85% absorbed by both the open water ocean and the non-snow covered land, a major change in the radiation feedback
mechanisms, accelerating warming and major changes in weather patterns.
about 85% reflected to about 85% absorbed by both the open water ocean and the non-snow covered land, a major change in the radiation feedback
mechanisms, accelerating warming and major changes in weather patterns.
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Ilulissat Region of Greenland
IlulissatGlacier
Il li tIlulissatFjord
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Ilulissat Glacier: Major Calving EffectIlulissat Glacier: Major Calving Effect
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Scale is over kilometer across the face and about 900 meters highScale is over kilometer across the face and about 900 meters high
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Wh f h hWh f h hWhat are some of the other consequences for the Arctic Region?
What are some of the other consequences for the Arctic Region?
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Methane Bogs in Siberia
QuickTime™ and aH 264 decompressorH.264 decompressor
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Shifting patterns in weather types and
locations. Thunderstorms have migrated
northward, along with lightningwith lightning,
which apparently caused the first known wildfire
north of the Brooks Range occurred g
last summer.
15
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Th hiftThese shifts are governed by (1)changes in oceanic Climate temperatures, (2) salinity, (3)nutrients, (4)changing
driven changes in
marine changing patterns in North Atlantic Deep Water formation,
a eecosystems.
and (5)interspecies interactions.
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The sea and inland ice is changing rapidly and disappearing inThe sea and inland ice is changing rapidly and disappearing in places essential to indigenous residents of the Arctic.
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In Summary:• Warming of the climate system is unequivocal as is now• Warming of the climate system is unequivocal, as is now
evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global average sea level.
• There is now higher confidence in projected patterns of i d th i l l f t i l diwarming and other regional-scale features, including
changes in wind patterns, precipitation and some aspects of extremes and of ice.p
• Anthropogenic warming and sea level rise will continue for centuries due to the time scales associated with li t d f db k if hclimate processes and feedbacks, even if greenhouse gas
concentrations were to be stabilized.What can we sayWhat can we sayWhat can we say about the future?What can we say about the future?
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(Purpose of C-ROADS(Climate Rapid Overview And Decision Support)
• Improve understanding of important climate• Improve understanding of important climate dynamics among:
PolicymakersyEducatorsThe public
• A climate model that is designed to help ensure that climate policy is informed by accepted, peer-reviewed sciencereviewed science
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An Assessment of Current Copenhagen (CoP 15) Proposals by
An Assessment of Current Copenhagen (CoP 15) Proposals byCopenhagen (CoP 15) Proposals by the 192 Countries of the UNFCCC
Copenhagen (CoP 15) Proposals by the 192 Countries of the UNFCCC
EU - Emissions 80% below 1990 by 2050
Brazil - 10-20% reduction of 2004 by 2020
China - Reduce emissions intensity 20% by 2020
South Africa - 40% below 2003 by 2050
2020US (Warn-Lieb) -71% below 2005 by 2050
Other Latin America - bau
India - Reduce emissions intensity 20% by 2020
Other Africa - bau
2020Russia - 1990 levels
Mexico - 10% below 2004 by 2014
Other Asia -Reduce emissions intensity 20% by
Global Deforestation - bau
2020
Canada - 20% below 2006 by 2020
Middle East - bau OECD Pacific -60% below 2000 by 2050 (AUS)
Afforestation - bau
2020 by 2050 (AUS)
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The Publicly Known Proposals to Reduce Emissions as of September 2009 Drops CO2 Concentrations from 950 ppm to
The Publicly Known Proposals to Reduce Emissions as of September 2009 Drops CO2 Concentrations from 950 ppm to
1000.00
about 700 ppm (The Target is 450 ppm of less) about 700 ppm (The Target is 450 ppm of less)
700 00
800.00
900.00 BAU
Sept 09
500.00
600.00
700.00Proposals
200.00
300.00
400.00
0.00
100.00
1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 21001900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Source: Climate Action Initiative using C-ROADS and SI Analysis of the Current Proposals
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The Publicly Known Proposals to Reduce Emissions as of September 2009 Yields an Average Global Temperature from the Business As Usual (BAU) of
4 50 oC (over 7 oF) by 2100 to about 3 5 oC above Pre-Industrial
The Publicly Known Proposals to Reduce Emissions as of September 2009 Yields an Average Global Temperature from the Business As Usual (BAU) of
4 50 oC (over 7 oF) by 2100 to about 3 5 oC above Pre-Industrial
4 50
5.00
BAU
4.50 C (over 7 F) by 2100 to about 3.5 C above Pre-Industrial4.50 C (over 7 F) by 2100 to about 3.5 C above Pre-Industrial
3.50
4.00
4.50
Sept 09Proposals
2.50
3.00
3.50
1.50
2.00
0.50
1.00
0.00
1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Source: Climate Action Initiative using C-ROADS and SI Analysis of the Current Proposals
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Sea Level Rise Projected for the Current Proposals by the 192 FNCCC Nations
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The question is: At what temperature will we stabilize?
750 ppm ~ 4.3 0CIPCC (2007) Forecast
550 ppm ~ 3 0C
450 ppm 2 0C450 ppm ~ 2 0C
There is the potential that the climate is likely, as projected byas projected by
the IPCC, to take humankind
where it has never been
17
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Climate change is no Climate change is no glonger simply an
environmental issue it is
glonger simply an
environmental issue it isenvironmental issue, it is an issue of economic security as well a an
environmental issue, it is an issue of economic security as well a ansecurity as well a an
equity issue for human ll b i h li
security as well a an equity issue for human
ll b i h liwell-being. The policy challenges are
well-being. The policy challenges are
Thank You !extraordinarily difficult!extraordinarily difficult!
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The Model
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C-ROADS Model Structure
(3 7 or 15 blocs)
User Input
SeaSpecific country Carbon
Total fossil fuel CO2
(3, 7, or 15 blocs)
Cli t
Other GHGs
TempSea
Level risecountry
emissionsCarbon cycleemissions
Net CO2 emissions
GHGs in atm
Climate
from forestsDeforestationAfforestation Forests
User Input
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The Simulation Produces Atmospheric CO2 Levels Consistent with IPCC and other Scenarios
The Simulation Produces Atmospheric CO2 Levels Consistent with IPCC and other ScenariosConsistent with IPCC and other ScenariosConsistent with IPCC and other Scenarios
Atmospheric CO2 Projected1,000 BERN ISAM A1FI
750
500ppm
BERN ISAM B1
250
0
MAGICC WRE(C-ROADS results in blue)
01850 1875 1900 1925 1950 1975 2000 2025 2050 2075 2100
Time (Year)
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Conclusion of Scientific Review Panel
The C-ROADS model: • “reproduces the response properties of state-of- the-art three
dimensional climate models very well”
• “is a sensitivity tool rather than a tool to provide precise• “is a sensitivity tool, rather than a tool to provide precise quantitative estimates of projected emissions, CO2concentrations, and temperature and sea level responses.”
• “Given the model’s capabilities and its close alignment with a f i bli h d i th F th A trange of scenarios published in the Fourth Assessment
Report of the IPCC we support its widespread use among policy makers and the general public.”
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Simulator Helps Users Conduct Customized Tests: What If ?Tests: What If…..?
Regional FF Emissions6 B
Regional FF Emissions6 B
Regional FF Emissions10 B
Business as usual4.5 B
3 B
Tons
C/y
ear
4.5 B
3 B
Tons
C/y
ear
All reduced 80% by 2050? Or by 2030?7.5 B
5 B
Tons
C/y
ear
Business as usual
1.5 B
02007 2023 2038 2054 2069 2085 2100
Time (year)
1.5 B
02007 2023 2038 2054 2069 2085 2100
Time (year)
2.5 B
02007 2023 2038 2054 2069 2085 2100
Time (year)
Regional FF Emissions6 B
4.5 B
Regional FF Emissions6 B
4.5 B
Regional FF Emissions6 B
4.5 BSome by 2030 d th 2060?
Starting in 2018?Developed acts but undeveloped
3 B
1.5 B
Tons
C/y
ear
3 B
1.5 B
Tons
C/y
ear
3 B
1.5 B
Tons
C/y
earand others 2060? doesn’t?
02007 2023 2038 2054 2069 2085 2100
Time (year)
02007 2023 2038 2054 2069 2085 2100
Time (year)
02007 2023 2038 2054 2069 2085 2100
Time (year)
(all graphs fossil fuel emissions)