4°c global warming: gg regional patterns and timing · • 4°c global warming (relative to...
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4°C global warming:
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g gregional patterns and timing
Richard Betts, Mike Sanderson, Debbie Hemming, Mark New, Jason Lowe, Chris Jones
4°C+ conference, Oxford University, 25.9.09
IPCC SRES emissions scenarios
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Van Vuuren and Riahi (2008)
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Model projections of global warming with IPCC SRES emissions scenarios
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Comparison of SRES scenarios with actual emissions
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Van Vuuren and Riahi (2008)
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Using climate model ensembles to assess confidence in projections
• Multi-model ensemble: set of (mostly) different models • IPCC 4th Assessment Report (AR4) – 23 models
• Perturbed physics ensembles: set of variants of one model• ClimatePrediction.net – HadCM3 model (1500+ variants)
• Met Office Hadley Centre (MOHC) “QUMP” project – HadCM3 model (17 variants)
Si l li t d l t d t th b l d l
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• Simple climate model tuned to the above complex models• IPCC “likely range of warming” statements
• Combination of the above• UKCP09 – mostly HadCM3, with some input from IPCC AR4 models
A1B scenario
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Global warming with A1B scenario: all IPCC models
“High end”:High-end : simulations with 4°C warming by by 2090s
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Pattern of warming by 2090s, A1B Mean of “high-end” IPCC simulations (3 models, mean global warming 4.3°C)
© Crown copyright Met OfficeTemperature change (°C) relative to 1961-1990
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Precipitation changes by 2090s, A1BMean of “high-end” IPCC simulations (3 models, mean global warming 4.3°C)
© Crown copyright Met OfficePrecipitation change (%) relative to 1961-1990
Global warming with A1B scenario: MOHC ensemble
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Pattern of warming by 2090s, A1BMean of “high-end” MOHC simulations (9 simulations, mean global warming 4.6°C)
© Crown copyright Met OfficeTemperature change (°C) relative to 1961-1990
Precipitation changes by 2090s, A1BMean of “high-end” MOHC simulations (9 simulations, mean global warming 4.6°C)
© Crown copyright Met OfficePrecipitation change (%) relative to 1961-1990
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A1FI scenarioscenario
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Pattern of warming by 2090s, A1FIMean of “high-end” MOHC simulations (14 simulations, mean global warming 5.4°C)
© Crown copyright Met OfficeTemperature change (°C) relative to 1961-1990
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Precipitation changes by 2090s, A1FIMean of “high-end” MOHC simulations (14 simulations, mean global warming 5.4°C)
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Global warming with A1FI scenario: MOHC ensemble
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Importance of carbon sinks for slowing CO2 rise
Emissions
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Change in atmospheric concentration
IPCC (2007)
The free ecosystem service that has been buying us time may not last…
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Gt C
) Carbon uptake by plants in 20th
century has buffered the past
–50
0
50
oval
s fr
om a
tmos
pher
e (G y p
CO2 rise
But climate change
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–150
–100
50
1950 2000 2050 2100
Car
bon
rem
o
vegetation carbonsoil carbon
1900
may put this into reverse
Cox et al (2000)
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Effects of climate-carbon cycle feedbacks on atmospheric CO2 rise
1000 with CO2-climate feedbacks1000
800
600
without CO2-climate feedbacks
cent
ratio
ns (p
pmv) IS92a “business-as-usual” scenario
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400
2001900 1950 2000 2050 2100
CO
2co
nc
Cox et al (2000)
Multi-model assessment of carbon cycle feedbacks (C4MIP): A2 emissions scenario
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Friedlingstein et al (2006)
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Global mean temperature: SRES A1FI
Range of global warming projections for A1FI (high emissions) scenario, including carbon cycle feedbacks
Simple model tuned to complex models, consistent with IPCC method
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5
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7
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ove
pre-
indu
stria
l
90th %ile
10th %ile
median
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0
1
2
1980 2000 2020 2040 2060 2080 2100
Year
o C ab
o
Exceedance of global warming thresholds, A1B, no carbon cycle feedbacks: ClimatePrediction.net
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Conclusions
• Current CO2 emissions are near (but not above) upper end of IPCC iscenarios
• 4°C global warming (relative to pre-industrial) is possible by the 2090s, especially under high emissions scenario
• Many areas could warm by 10°C or more
• The Arctic could warm by 15°C or more
• Annual precipitation could decrease by 20% or more in many areas
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• Annual precipitation could decrease by 20% or more in many areas
• Carbon cycle feedbacks expected to accelerate warming
• With high emissions, best guess is 4°C in 2070s
• Plausible worst case: 4°C by 2060