© Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

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Presentation transcript:

© Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre

© Crown copyright Met Office Australia January 2013

© Crown copyright Met Office Hobart, Tasmania, 4 th January 2013

© Crown copyright Met Office Dunalley, 4 th January 2013

© Crown copyright Met Office Dunalley, 4 th January 2013

© Crown copyright Met Office Australia’s “angry summer”

© Crown copyright Met Office Britain’s washout Summer : 2012 Diamond Jubilee, 3 rd June, Reading

Why is climate changing ? How is extreme weather changing ? Is it possible to link recent extreme weather like the Australian heatwave or the wet British summer to climate change ? © Crown copyright Met Office

The climate is warming © Crown copyright Met Office Annual mean temperature ( )

Concentrations of carbon dioxide and other greenhouse gases are increasing © Crown copyright Met Office

The greenhouse effect © Crown copyright Met Office

The oceans have warmed and sea level has risen.

The climate system has continued to accumulate energy during the last 15 years Box 3.1 Fig 1

© Crown copyright Met Office

IPCC Fifth Assessment Report

Observed decadal mean warming Fig SPM.5

Observed warming inconsistent with that expected from natural factors Fig SPM.5

Observed warming consistent with simulations that include anthropogenic factors Fig SPM.5

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed The observed warming 1951− 2010 is approximately 0.6°C to 0.7°C. Fig. TS.10

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed Fig. TS.10 The observed warming 1951− 2010 is approximately 0.6°C to 0.7°C.

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed Fig. TS.10 The observed warming 1951− 2010 is approximately 0.6°C to 0.7°C.

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed Fig. TS.10 The observed warming 1951− 2010 is approximately 0.6°C to 0.7°C.

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed Fig. TS.10 The observed warming 1951− 2010 is approximately 0.6°C to 0.7°C.

Global mean warming since 1951 (°C) Solar, Volcanic Aerosols CO 2, CH 4, N 2 O Anthropogenic Internal Variability Observed It is extremely likely that human influence has been the dominant cause of the observed warming since the mid-20th century. Fig. TS.10

IPCC Summary for Policy Makers agreed line by line in Stockholm, September 2013, by 110 governments

© Crown copyright Met Office Why is climate changing ? How is extreme weather changing ? Is it possible to link recent extreme weather like the Australian heatwave or the wet British summer to climate change ? © Crown copyright Met Office

Was Australia’s “angry summer” due to anthropogenic climate change ?

© Crown copyright Met Office It isn’t possible to say a particular extreme season was or was not due to anthropogenic climate change.

© Crown copyright Met Office Human influence has very likely at least doubled the probability of European summer temperatures as hot as Stott et al, Nature, But it is possible to evaluate how the odds of such an event have changed.

© Crown copyright Met Office Change in Extremes in warming climate Temperature now Probability of occurrence Hot temperature extremes Cold temperature extremes E. Palin Temperature in future Fewer cold extremes More hot extremes More record hot extremes Cold threshold AverageHot threshold New average

© Crown copyright Met Office Such extreme summer temperatures as 2013 very likely at least 2.5 times more probable due to human influence. Lewis et al, GRL, This has also now been done for the Australian summer of 2012/13.

© Crown copyright Met Office Explaining extreme climate and weather events of the previous year from a climate perspective Tom Peterson, Martin Hoerling, Peter Stott, Stephanie Herring.

© Crown copyright Met Office Extreme eventEvidence for anthropogenic influence ? US heatwaveYES Hurricane Sandy storm surgeYES September Arctic sea ice minimumYES February European cold spellNO Wet UK summerNO Iberian winter droughtYES Rainfall deficitits in Eastern Kenya and Southern Somaliia NO North China floods, JulyNO Heavy rainfall in Southwestern Japan, July NO Extreme rainfall over Eastern Australia, March YES Extreme rainfall, Goldan Bay, New Zealand, December 2011 YES US droughtNO

© Crown copyright Met Office Summer 2012 Wettest since 1912

© Crown copyright Met Office Long term natural cycle Atlantic sea surface temperature Shifts jet stream Summer 2012

Iberian winter drought Trigo et al, 2013 A tendency towards a drier Mediterranean driven by anthropogenic emissions of greenhouse gases and aerosols, although modulated by the North Atlantic oscillation

The North Atlantic Oscillation © Crown copyright Met Office

The North Atlantic Oscillation © Crown copyright Met Office Winter 2009/2010

Rainfall patterns are projected to continue to change leading to more frequent droughts in some regions and more floods in others. © Crown copyright Met Office

Arctic sea ice in September could be gone by 2050 © Crown copyright Met Office

Sea level rise will continue © Crown copyright Met Office

The extent of climate change depends on future greenhouse gas emissions © Crown copyright Met Office

Human influence on the climate system is clear Better understanding of the changing risks of extreme weather will help people cope with the effects of anthropogenic climate change. Extreme weather and seasons result from the interplay of natural climate variability and anthropogenic climate change. At the Met Office we are developing an “operational attribution” system to assess the risks of such extremes on a regular basis. A new annual report provides puts extreme weather from last year in different regions of the world into the context of natural climate variability and anthropogenic climate change. © Crown copyright Met Office