latest climate scienceimplications for wales met office september 2013

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Latest climate science Implications for Wales © Crown copyright Met Office Vicky Pope Sept 2013

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Latest climate science Implications for Wales a presentation by Vicky Pope, Met Office.

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Page 1: Latest climate scienceImplications for Wales Met Office September 2013

Latest climate scienceImplications for Wales

© Crown copyright Met Office

Vicky Pope

Sept 2013

Page 2: Latest climate scienceImplications for Wales Met Office September 2013

© Crown copyright Met Office

Latest climate scienceImplications for Wales

• Basics of climate – theory and observations

• Why has there been such extreme weather recently?

• Is this the sign of things to come? Impact on projections

Page 3: Latest climate scienceImplications for Wales Met Office September 2013

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Page 4: Latest climate scienceImplications for Wales Met Office September 2013

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Heat energy re-emitted to warm Earth

Heat energy passes through atmosphere

Heat energy radiated from Earth

Sun’s energy absorbed by atmosphere

Sun’s energy reflected by Earth

Sun’s energy reflected by clouds

Incoming energy from the sun

Page 5: Latest climate scienceImplications for Wales Met Office September 2013

© Crown copyright Met Office© Crown copyright Met Office

Water evaporates from rivers lakes and the ocean

Water condenses to form clouds

Loss of water from plants, soil, animals and people

Water returns to land as precipitation

Water carried downhill by rivers

Water seeps into ground and flows to sea

Page 6: Latest climate scienceImplications for Wales Met Office September 2013

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Hadley cell

Ferrel cell

Polar cell

Trade winds

Page 7: Latest climate scienceImplications for Wales Met Office September 2013

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Page 8: Latest climate scienceImplications for Wales Met Office September 2013

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Page 9: Latest climate scienceImplications for Wales Met Office September 2013

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Evidence: the Greenhouse effect

The average temperature of the Earth is 14 ºC. Without the blanket of greenhouse gases it would be –18 ºC.

The water vapour feedback enhances the warming due to man-made greenhouse gases

Page 10: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Atmospheric carbon dioxide

1850 1900 1950 2000

380

360

340

320

Atmospheric carbon dioxideA

tmos

phe

ric c

arb

on d

ioxi

de

(par

ts p

er m

illio

n)

CO2 has risen by 107ppm (38%) from pre-industrial levels of 280ppm.

Page 11: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Land surface temperature

Global temperatures have increased decade on decade since the mid 20th century, consistent with the basic physics.

The water vapour feedback enhances the warming due to man-made greenhouse gases

1850 1900 1950 2000

Page 12: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Sea surface temperature

1850 1900 1950 2000

Page 13: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Tropospheric temperature

1850 1900 1950 2000

Page 14: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Specific humidty

1850 1900 1950 2000

Page 15: Latest climate scienceImplications for Wales Met Office September 2013

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INCREASING – Sea level

1850 1900 1950 2000

Page 16: Latest climate scienceImplications for Wales Met Office September 2013

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DECREASING – September Arctic sea ice extent

1850 1900 1950 2000

Page 17: Latest climate scienceImplications for Wales Met Office September 2013

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DECREASING – Glacier mass balance

1850 1900 1950 2000

Page 18: Latest climate scienceImplications for Wales Met Office September 2013

Why has there been such extreme weather recently?

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Christidis and Stott, Met OfficeMassey et al, University of Oxford, Met Office

• The odds of the cold December 2010 temperatures have halved as a result of human-induced climate change

• Unusual circulation patterns can still bring very cold winter months

UK cold winter December 2010 Coldest December on record in Wales -3.8 degCRecord minimum: -18.0 deg C at Llysdinam (Powys) 28 November 2010

Page 20: Latest climate scienceImplications for Wales Met Office September 2013

Oct 2010 – March 2012 Rainfall% of 1971-2000 average

2 dry winters

Extreme weatherFrom drought...

Page 21: Latest climate scienceImplications for Wales Met Office September 2013

Summer 2012 Rainfall% of 1971-2000 average

2 dry winters

Extreme weather...to flood

Wettest June on record (180% of average)

3rd wettest summer on record for Wales (240% of average)

Page 22: Latest climate scienceImplications for Wales Met Office September 2013

Is this the sign of things to come? Impact on projections

Page 23: Latest climate scienceImplications for Wales Met Office September 2013

Representative comparison between CMIP3 and 5

models (scaled using simple models)

Climate model projections CMIP5Global surface temperature (single study, AR5 will contain synthesised results)Knutti and Sedláček, 2013

Page 24: Latest climate scienceImplications for Wales Met Office September 2013

Climate model projections CMIP5Preciptation (single study, AR5 will contain synthesised results)Knutti and Sedláček, 2013

December - February

June - August

Stippling – high robustnessHatching – no significant changeWhite – models inconsistent

Page 25: Latest climate scienceImplications for Wales Met Office September 2013
Page 26: Latest climate scienceImplications for Wales Met Office September 2013

Important processes for UK weather and climate

• North Atlantic weather – slow changes in ocean surface temperatures

• Tropical Pacific weather – El Nino• Arctic Sea ice retreat• Solar variability

Atlantic Multidecadal Oscillation

Video of the jet streamhttp://www.metoffice.gov.uk/learning/wind/what-is-the-jet-stream?rel=0

Page 27: Latest climate scienceImplications for Wales Met Office September 2013

Low UV from the sun leads to easterly winds and cold conditions in Europe and the US

Page 28: Latest climate scienceImplications for Wales Met Office September 2013

Global focus

Page 29: Latest climate scienceImplications for Wales Met Office September 2013

Global average temperatures (including latest observations)

Page 30: Latest climate scienceImplications for Wales Met Office September 2013

Hiatus in warming: Possible contributions Met Office Hiatus report (IPCC AR5 will contain synthesised results) http://www.metoffice.gov.uk/research/news/recent-pause-in-warming

• Natural variability: models have 10-15 year periods with no warming or even cooling

• Incoming radiation: reduction of 0.6 Wm-2 needed to explain pause. Maximum possible is 0.3 Wm-2

• Recent decrease in stratospheric water vapour: traps less heat: up to 0.1Wm-2

• Change in man-made aerosols: little net effect

• Volcanic eruptions: not enough during period

• Extended solar minimum: less than 0.2Wm-2

• Ocean changes: could be a major contributor • Ocean heat content, sea-level rise observations: Earth system continued

to absorbed heat

• Additional heat appears to have been absorbed in the ocean.

• Increased exchange to deep ocean appears to have caused at least part of the pause in surface warming,

• Observations indicate that Pacific Ocean may play a key role.

Page 31: Latest climate scienceImplications for Wales Met Office September 2013

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The impact of a global temperature rise of 4 ºC

Change in temperature from pre-industrial climate

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16

Current City population • 3-10 million • 10-20 million

Meltingice

OceanAcidification

Rainforestloss

Reduced crops

Forestfire

Increased drought

Stronger tropical storms

Methane release

More heatwaves

Page 32: Latest climate scienceImplications for Wales Met Office September 2013
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Steadily increasing CO2 (similar to BAU scenario by 2100). Excludes deforestation and fire

Page 34: Latest climate scienceImplications for Wales Met Office September 2013

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Represent the earth by a grid of squares, typically of length 100 km or smaller. Atmosphere and oceans are divided into vertical slices of varying depths. 3-dimensional picture of the state of the atmosphere and oceans. Integrate equations of motion and thermodynamics forward in time. Conserve heat, moisture, salinity and momentum

Fundamentals of weather and climate modelling

Page 35: Latest climate scienceImplications for Wales Met Office September 2013

Best long-term climate models, UKCP09

State-of-art seasonal

model

Current global weather forecasting

Current UK weather

forecasting + ground-breaking

climate work

Mountains (130km grid)

Mountains (60km grid)

1.5km resolution climate modelResolution of Welsh terrain

Mountains (25km grid)

Mountains (1.5km grid)

Page 36: Latest climate scienceImplications for Wales Met Office September 2013

Important processes

Rainfall Oct to March

Video of the jet streamhttp://www.metoffice.gov.uk/learning/wind/what-is-the-jet-stream?rel=0

Page 37: Latest climate scienceImplications for Wales Met Office September 2013

Sea Ice

Page 38: Latest climate scienceImplications for Wales Met Office September 2013

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