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

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

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

Page 1: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

© Crown copyright Met Office

Extreme weather and climate changeDr Peter Stott, Met Office Hadley Centre

Page 2: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

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AustraliaJanuary 2013

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Hobart, Tasmania, 4th January 2013

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Dunalley, 4th January 2013

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Dunalley, 4th January 2013

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Australia’s “angry summer”

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Britain’s washout Summer : 2012

Diamond Jubilee, 3rd June, Reading

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• 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 ?

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The climate is warming

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Annual mean temperature (1901-2012)

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Concentrations of carbon dioxide and other greenhouse gases are increasing

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The greenhouse effect

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The oceans have warmed and sea level has risen.

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The climate system has continued to accumulate energy during the last 15 years

Box 3.1 Fig 1

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IPCC Fifth Assessment Report

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Observed decadal mean warming

Fig SPM.5

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Observed warming inconsistent with that expected from natural factors

Fig SPM.5

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Observed warming consistent with simulations that include anthropogenic factors

Fig SPM.5

Page 19: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

The observed warming 1951− 2010 isapproximately 0.6°C to 0.7°C.

Fig. TS.10

Page 20: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

Fig. TS.10

The observed warming 1951− 2010 isapproximately 0.6°C to 0.7°C.

Page 21: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

Fig. TS.10

The observed warming 1951− 2010 isapproximately 0.6°C to 0.7°C.

Page 22: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

Fig. TS.10

The observed warming 1951− 2010 isapproximately 0.6°C to 0.7°C.

Page 23: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

Fig. TS.10

The observed warming 1951− 2010 isapproximately 0.6°C to 0.7°C.

Page 24: © Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.

Global mean warming since 1951 (°C)

Solar, Volcanic

Aerosols

CO2, CH4, N2O

Anthropogenic

Internal Variability

Observed

It is extremely likely that human influence hasbeen the dominant cause of the observed

warming since the mid-20th century.

Fig. TS.10

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

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• 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

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

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It isn’t possible to say a particular extreme season was or was not due to anthropogenic climate change.

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Human influence has very likely at least doubled the probability of European summer temperatures as hot as 2003. Stott et al, Nature, 2004.

But it is possible to evaluate how the odds of such an event have changed.

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Change in Extremes in warming climate• Temperature now

Probability of occurrence

Hot temperature

extremesCold temperature

extremes

E. Palin

• Temperature in future

Fewer cold

extremes

More hot extremes

More record

hot extremes

Cold threshold

Average Hot threshold

New average

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Such extreme summer temperatures as 2013 very likely at least 2.5 times more probable due to human influence. Lewis et al, GRL, 2013.

This has also now been done for the Australian summer of 2012/13.

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Explaining extreme climate and weather events of the previous year from a climate perspective

Tom Peterson, Martin Hoerling, Peter Stott, Stephanie Herring.

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Extreme event Evidence for anthropogenic influence ?

US heatwave YES

Hurricane Sandy storm surge YES

September Arctic sea ice minimum YES

February European cold spell NO

Wet UK summer NO

Iberian winter drought YES

Rainfall deficitits in Eastern Kenya and Southern Somaliia

NO

North China floods, July NO

Heavy rainfall in Southwestern Japan, July

NO

Extreme rainfall over Eastern Australia, March

YES

Extreme rainfall, Goldan Bay, New Zealand, December 2011

YES

US drought NO

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Summer 2012 Wettest since 1912

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• Long term natural cycle

• Atlantic sea surface temperature

• Shifts jet stream

Summer 2012

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Iberian winter droughtTrigo 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

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The North Atlantic Oscillation

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The North Atlantic Oscillation

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Rainfall patterns are projected to continue to change leading to more frequent droughts in some regions and more floods in others.

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Arctic sea ice in September could be gone by 2050

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1950 2000 2050 2100

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Sea level rise will continue

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The extent of climate change depends on future greenhouse gas emissions

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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.

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