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Gian-Kasper Plattner
Head WGI TSU
University of Bern
IPCC 5th Assessment Cycle (2008-2014):
Human influence on the
climate system is clear.
Continued GHG emissions will
cause further warming and
amplify existing risks.
Changes in climate have
caused impacts in natural
and human systems.
Multiple pathways exist to likely
limit warming to below 2°C.
Warming of the climate system
is unequivocal
IPCC2013,Fig.SPM.1b;IPCC2014,Fig.1.1
Anomaly(°C)relativeto1961-1990
EnergyContent(1021Joule)
1980 1990 2000 2010
300
200
0
100
-100
1970
Ocean warming dominates the increase
in energy stored in the climate system
IPCC2013,Box3.1Fig.1;IPCC2014,Fig.1.2
Human influence on the climate system is clear,
and recent anthropogenic emissions of
greenhouse gases are the highest in history.
IPCC2014,Fig.SPM.1c,d
IPCC2013,Fig.SPM.7;IPCC2014,Fig.SPM.6
Global surface temperature change for the end of
the 21st century is likely to exceed 1.5°C relative
to 1850−1900 for all scenarios except RCP2.6.
Global mean surface temperature change from 1986-2005
IPCC2013,Fig.SPM.8,IPCC2014,Fig.SPM.7
Further warming will increase the likelihood of
severe, pervasive and irreversible impacts for
people and ecosystems.
Change in average surface temperature (1986-2005 to 2081-2100)
RCP8.5
Global mean sea level will continue to rise
over the 21st century... and beyond..
IPCC2013,TFE.2,Fig.2
+19 cm
+63 cm
Climate change will amplify existing risks and
create new risks for natural and human systems.
IPCC2013,TFE.2,Fig.2
+19 cm
+63 cm
Global mean warming
All CO2 emissions since 1750
Global mean warming
All CO2 emissions since 1750
Warming of 0.8 to 2.5°C
1000 billion tons of carbon
Any climate target implies
a limited carbon budget
Budget for the 2°C target: 790 bill t C
CO2 emissions until 2014*: −545 bill t C
CO2 emissions in 2014*: 10.1 bill t C
Remaining emissions: 245 bill t C
*updatedfromIPCC2013,WGISPM
Limiting climate change would require substantial and
sustained reductions in greenhouse gas emissions which,
together with adaptation, can limit climate change risks.
2°C world
IPCC2013,Fig.SPM.8;IPCC2014Fig.SPM.7
4.5°C world2°C world
IPCC2013,Fig.SPM.8;IPCC2014Fig.SPM.7
4.5°C world2°C world
Today we have a choice.

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AR5 Synthesis Report - Working Group I Contribution

Editor's Notes

  1. All IPCC Assessment Reports are available at www.ipcc.ch
  2. Erwärmung oberste 75m von 1971-2010: 0.11 [0.09 to 0.13] °C per decade KW (zB Leibstadt): 7 TWh in einem Jahr. 500x current world energy consumption every year or 10 Mill modern nuclear power plant (1 KKW ca. 7 TWh in 1 year) Ocean warming dominates the increase in energy stored in the climate system, accounting for more than 90% of the energy accumulated between 1971 and 2010 (high confidence).
  3. AR5: TCR = 1.0 to 2.5 °C (likely range; high confidence); extremely unlikely larger than 3°C AR5: ECS = 1.5 to 4.5 °C (likely range; high confidence); extremely unlikely less than 1°C (high confidence); very unlikely greater than 6°C (medium confidence)
  4. AR5: TCR = 1.0 to 2.5 °C (likely range; high confidence); extremely unlikely larger than 3°C AR5: ECS = 1.5 to 4.5 °C (likely range; high confidence); extremely unlikely less than 1°C (high confidence); very unlikely greater than 6°C (medium confidence)
  5. AR5: TCR = 1.0 to 2.5 °C (likely range; high confidence); extremely unlikely larger than 3°C AR5: ECS = 1.5 to 4.5 °C (likely range; high confidence); extremely unlikely less than 1°C (high confidence); very unlikely greater than 6°C (medium confidence)
  6. bis 2011: 515 GtC (IPCC AR5) 2012: 9.6 GtC 2013: 9.9 GtC 2014: 10.1 GtC Total 534.5 GtC