geoffjenkins , new climate change scenarios

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  • 8/14/2019 GeoffJenkins , New Climate Change Scenarios

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    Sense about Science

    St Johns College Oxford, 17 March 2007

    New climate change scenarios for the UK

    Geoff Jenkins, Hadley Centre, Met Office, Exeter

    and

    Royal Meteorological Society, Reading.

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    2Met Office Hadley Centre

    Global temperatures 1850-2006 (+ 2007 forecast)

    Hadley Centre/UEA

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    3Met Office Hadley Centre

    Natural factors which can change climate

    Variations in the Earth's orbit

    (Milankovic effect)

    Stratosphericaerosol from

    energetic

    volcanoes

    Variations in the energy

    received from the sun

    Chaotic interactions in

    the Earth's climate

    (for example, El Nino, NAO)

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    4Met Office Hadley Centre

    Emissions of CO2 from fossil-fuel burning;rapid rise since 1950

    Source: CDIAC, ORNL

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    5Met Office Hadley Centre

    Atmospheric concentration of carbon dioxide

    1800 1900 2000

    375

    350

    325

    300

    275

    Carbon dioxide

    concentration in

    parts per million

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    6Met Office Hadley CentreSource: Intergovernmental Panel on Climate Change (IPCC)

    1.0

    0.5

    0

    1900 1950 2000

    Temp

    eraturechange

    CObservations

    Model

    simulations withnatural variability

    plus mans

    activities

    Model

    simulations

    with only

    natural

    variability

    Models can only simulate recent change whenhuman factor are included

    Source: IPCC AR4

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    7Met Office Hadley Centre

    Central England Temperature 1772-2006

    2006 was easily the warmest year in England.The warming of nearly 1degC since 1980 cannot be explained by natural factors

    and is consistent with the expected response to human factors.

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    8/218Met Office Hadley Centre

    Emissions to 2000, and IPCC projections to 2100

    1850 1900 1950 2000 2050 2100

    30

    20

    10

    0

    Fossil-fuelemissio

    ns

    GtC/y

    High (SRES A1FI)

    Medium-High (A2)

    Medium-Low (B2)

    Low (SRES B1)

    Source: CDIAC and IPCC

    Problem: we do not know

    the relative likelihood of

    each emission scenario

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    9/219Met Office Hadley Centre

    Global average temperature rise UK model

    Globaltemperatureri

    se,

    degreesC High emissions

    Medium-high emissions

    Medium-low emissions

    Low emissions

    Start to diverge

    from 2040s

    Red bar =

    likely range

    from all

    climate

    models

    Blackbar =

    best

    estimate

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    10/2110Met Office Hadley Centre

    Planning adaptation to climate change in the UK

    Adaptation planners, eg: Transport (road, rail) Environment Agency Utilities (water, energy)

    Insurance Local Government Government Regulators Many others

    UK

    Climate

    Impacts

    Programme,

    Oxford

    other

    adaptationtools& advice

    ClimateChange

    Scenarios

    Met OfficeHadley Centre

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    11/2111Met Office Hadley Centre

    2002 Climate change scenarios (UKCIP02)

    50km resolution from Hadley

    Centre GCM and RCM

    4 future emissions scenarios Starting to be used by

    private and public-sector to

    plan adaptation (eg EA 20%

    uplift of winter river flow)

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    12/2112Met Office Hadley Centre

    winter summer

    C

    Change in UK temperature by the 2080sMedium High emissions scenario

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    13/2113Met Office Hadley Centre

    winter summer

    %

    Change in UK precipitation by the 2080sMedium High emissions scenario

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    14/2114Met Office Hadley Centre

    UK snowfall will be greatly reduced

    % reduction in snowfall by 2080sSnowman

    February 2007

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    15/2115Met Office Hadley Centre

    Modelling uncertainties IPCC 4AR (2007)

    Problem: we do not know the relative likelihood of each prediction

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    16/2116Met Office Hadley Centre

    Next scenarios: Moving from uncertainty to probability

    current situation future situation

    2080s SE England summer rainfall

    -50% -40% -30% -20% -10% 0% +10%

    Probability

    -50% -40% -30% -20% -10% 0% +10%

    2080s SE England summer rainfall

    Probability

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    17/2117Met Office Hadley Centre

    UK climate is warmed by the Gulf Stream Ocean currents can be affected by climate change

    Rapid cooling 11 000 years ago due to Gulf Stream shutdown

    Could this happen again due to human activity?

    Could the Gulf Stream switch off?

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    18/2118Met Office Hadley Centre

    How the Gulf stream is maintained

    Warm surface current

    Cold deep current

    Convection areas

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    19/2119Met Office Hadley Centre

    Gulf Stream collapse would mean a cold UK

    UK: 3-5C cooling

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    20/2120Met Office Hadley Centre

    Gulf Stream: predicted to decline but not switch off

    Circulationstr

    ength(Sv)

    High emissions

    Medium-HighMedium LowLow Emissions

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    21/21Met Office Hadley Centre

    Summary

    Very likely that human activities, mainly fossil fuel burning,are to blame for most of the last 50yr warming

    Cannot explain Central England warming by natural factors

    Even with strong mitigation policies, climate will change, so

    scenarios are needed by planners to prepare for adaptation. Scenarios generated for UK Climate Impacts programme in

    2002 have been widely used to explore possible responses.

    But climate models give very different predictions for local

    regions and for extremes; difficult for planners. Next set of scenarios will handle this uncertainty by being

    probabilistic in nature.