IPCC Working Group I: The Physical Science Basis Thomas Stocker Co-Chair Working Group I University of Bern, Switzerland Gian-Kasper Plattner Deputy Head, Director of Science TSU WGI, University of Bern The Physical Science Basis of Climate Change: Latest Findings to be Assessed by WGI in AR5
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IPCC Working Group I: The Physical Science Basis
Thomas StockerCo-Chair Working Group I
University of Bern, Switzerland
Gian-Kasper PlattnerDeputy Head, Director of Science
TSU WGI, University of Bern
The Physical Science Basis of Climate Change: Latest Findings to be Assessed by WGI in AR5
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
Warming in the climate system is unequivocal...
(IPCC, 2007, Fig. SPM-3)
IPCC (2007):
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(IPC
C, 2
007,
Fig
. WG
I-SPM
-4)
Most of the observed increase in global averaged temperature ... is very likely due to ... increase in GHG concentrations.
IPCC (2007):
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(IPC
C, 2
007,
Fig
. WG
I-SPM
-6)
2020-2029 2090-2099
Change in Temperature (°C), Scenario A2
Continued GHG emissions ... would induce many changes ... that would very likely be larger than those observed ...
IPCC (2007):
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
Some policy-relevant findings to be assessed in AR5:
Observations (3 examples)
Projections (3 examples)
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
2009: 387 ppm
(Siegenthaler et al., 2005; Lüthi et al., 2008, NOAA)
1. CO2 : Higher levels and more rapid increase
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(Prit
char
d et
al.
2009
)
2. Extensive thinning on the margins of Greenland and Antarctica
Presenter
Presentation Notes
Data from satellite laser altimetry 2003-2007 glacier dynamics at ocean margins Greenland: changes now reach all latitudes Antarctica: intensifcation in key areas changes detectable even after decades since an event inward penetration of perturbations dynamic thinning now contributes 1.8 mm/yr to SLR
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(Merrifield et al., 2009, in BAMS)
3. Persistent sea-level rise consistent with earlier estimates
IPCC 2007:
Merrifield et al., 2009:
[1993–2003] (3.1 ± 0.7) mm/yr
[1993–2008] (3.5 ± 0.4) mm/yr
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
4. Rapid loss of Arctic sea ice
(Wan
g an
d O
verla
nd, 2
009)
ice-free
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(IPCC, 2007, Chapter 10, simplified, Plattner et al. 2008)
5. Long-term commitment and irreversibility of CO2 perturbation
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
(Rob
ock
et a
l., 2
008)
Year
ONOFF
10 Mio t Sulphur / Year
Termination Problem
6. Abrupt climate changes caused by geoengineering
Presenter
Presentation Notes
brown: 10Mt/yr into the tropical stratosphere secondary effects such as changes in precipitation patterns are largely unknown direct effects of CO2, such as ocean acidification, will proceed even under geoengineering schemes
Working Group I Contribution to the IPCC Fifth Assessment ReportThe Physical Science Basis: Latest Findings to be Assessed by WGI in AR5
Conclusions:
IPCC WGI firmly stands behind the conclusions of AR4, the community of researchers and its individuals providing the scientific basis, and the procedures of IPCC Assessments;
The combination of observations and paleoclimate information shows unprecedented changes in the climate system, both in amplitude and rate for 100‘s to many 1000‘s of years;
Wide-spread melting of ice margins is observed in Greenland and Antarctica with implications for sea level rise;
Emitted CO2 remains in the atmosphere for 1000‘s of years causing irreversible changes in the climate and in ocean chemistry;
Geoengineering methods have an inherent termination problemand do not mitigate the direct effects of CO2 increase.