the science of the uk climate projections · climate predictions including natural variability,...
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The science of the UK Climate ProjectionsProf. John Mitchell OBE FRS
Director of Climate Science, Met Office
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Basic Science-what every good sceptic ought to know
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CO2 Concentration in Ice Core Samples andProjections for Next 100 Years
150
200
250
300
350
400
450
500
550
600
650
700
Years Before Present
Vostok RecordIPCC IS92a ScenarioLaw Dome RecordMauna Loa Record
Current(2001)
Projected(2100)
0100,000200,000300,000400,000
CO
2C
once
ntra
tion
(ppm
v)
Current (and projected future) CO2 concentrations exceed those of the last 400,000yrs. Not like a natural cycle?
Projected (2100)500-900ppm
Current (2009)
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Physics of greenhouse effectChange in temperature (0C)for doubled carbon dioxide
• Temperature only 1.0 School physics
• Water vapour 2.0 Empirical, model, and analogue evidence
• Sea-ice, snow, clouds 1.5 – 5.5 Uncertainties due to modelling
feedbacks
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modelled temperature: natural plus human forcing
Observed temperatureModelled temperature
Observed temperatureModelled temperature
modelled temperature: natural forcing only
Is the observed change natural?
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modelled temperature: natural plus human forcing
Observed temperatureModelled temperature
Observed temperatureModelled temperature
modelled temperature: natural forcing only
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modelled temperature: natural plus human forcing
Observed temperatureModelled temperature
Observed temperatureModelled temperature
modelled temperature: natural forcing only
Need human effects to explain the obs record
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Global modelling
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Projections and uncertainties (1)
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Projections and uncertainties (2)
England &Wales Precipitation
Pre
cipi
tatio
n A
nom
oly
(mm
)
• Natural variability
Chaotic variations in circulation and long term cycles such as El Nino
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Adaptation – even 2C is not trivial
observationsMet Office Projections
2040s
2060sSo
uthe
rn E
urop
e Te
mpe
ratu
re a
nom
aly
(wrt
196
1-90
) °C
2003
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Regional climate changeand probabilistic
predictions
-UKCP09
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Moving from uncertainty to probability
UKCIP02 gave a single estimate of changes
Using many models in IPCC AR4 gave a range of estimated changes
UKCP09 uses over 400 model projections to give the probability of estimated changes
From frequency to probabilities
• Run climate model with several hundred variations of the models parameters
• Systematically cover parameter space using a statistical emulator
• Weight according to climate constraints
• Allow for differences with other climate models (IPCC AR4)
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From frequency to probabilities
Original model runsExtend with emulatorObservational constraintsTake account of other models
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Moving from a global to a regional scale
400 global climate projections
11 regional climate projections
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• High resolution regional projections account for the effects of coastlines, mountains, and other regional influences
Generating regional information
300km Global Model
25km Regional Model
50km Regional Model
5km Observed
Winter precipitation for 1961-2000, mm/day
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Contributions to uncertainty
931
2535
Natural Variability Carbon Cycle
Downscaling Model Uncertainty
15
20
43
22
2020’s 2080’s(Winter rainfall in south east England)
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Giving probabilities
• UKCP09 provides probabilities which measure how strongly different outcomes for climate change are supported by current evidence(models, observations, understanding)
• We can make statements like “The central estimate is X, it is very likely to be higher than Y, and very likely to be lower than Z.”
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More confident projections
UKCIP02Single projection
Very unlikely to be less than (10%)
UKCP09Central estimate (50%)
Very unlikely to be more than (90%)
Sum
mer
Rai
nfal
l 208
0’s
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Climate over Eastern Scotland
0% 50% 90%
Winter temperature 0.7 1.7 2.9
Summer temperature 1.1 2.4 3.8 5.0
Winter precipitation (%) 2 10 20
Summer precipitation (%) -26 -12 1
2050s Medium Emissions
Sea Level
• The sea level in Edinburgh is expected to rise:
13.9 cm by 2050
24.4 cm by 2080
30.5 cm by 2095
Central estimates based on 1961-1990 baseline, medium emissions scenario
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A long-term vision for future UKCPsIntegrated weather and climate prediction for
estimating hazards and risk:
N x Global predictions at ~20km with lead
times of days to years:
Synoptic drivers
<N x Regional predictions at ~1km:
Local meteorology
PDF of local hazard:
Impacts
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Summary
• Climate is changing due to increases in greenhouse gases, and will continue to change
• There are a number of sources of uncertainty in climate predictions including natural variability, future emissions and limitations in modelling climate.
• Predictions at a regional scale are less certain that global scale- hence the need for a probabilistic approach
• UKCP09 accounts for major known sources of uncertainty in future projections, apart from common model errors
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Questions and answers
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How extreme weather will change
1980’s 2080’sTotal rainfall in an event with a 1 in 30 year return period
wet
ter
wet
ter
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Has global warming gone away?
Since 1998, the warmest year on record, observations have shown a levelling off of the warming signal.
Latest decadal prediction shows that global warming will reassert itself. Beyond 2010 at least half the years are expected to be warmer than 1998.
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Change in winter and summerprecipitation 1961–2006
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Not all change is human induced
1940 1960 1980 2000
−20
−10
0
10
20
30
40
50
0
% c
hang
e fr
om 1
961−
1990
ave
rage
NW Scotland December−MarchSE England July−August
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UK climate change+0.7°C now2008 More than doubled risk of heat waves2050 Glasgow - average increase 1.6ºC
Glasgow - hottest day increase 2.3 ºC
By the 2050s…
Eastern Scotland
Northern Scotland
Western Scotland
Summer averageTemperature
+ 2.3ºC + 2.0ºC + 2.4ºC
Winter average temperature
+ 1.7ºC + 1.7ºC + 1.9ºC
Summer precipitation
- 12% - 10% - 12%
Winter precipitation
+ 10% + 13% + 15%
If emissions continue at their present rate:
Central estimates based on 1961-1990 baseline
By the 2080s…
Eastern Scotland
Northern Scotland
Western Scotland
Summer averageTemperature
+ 3.5ºC + 3.0ºC + 3.5ºC
Winter average temperature
+ 2.3ºC + 2.2ºC + 2.6ºC
Summer precipitation
- 16% - 11% - 15%
Winter precipitation
+ 12% + 17% + 21%
If emissions continue at their present rate:
Central estimates based on 1961-1990 baseline
Information is available as maps
2020s, central estimate 2050s, central estimate 2080s, central estimate
change in annual average temperatures, ºC, medium emissions scenario
Users can compare differentemissions scenarios
2080s, central estimate, low emissions
2080s, central estimate, medium emissions
2080s, central estimate, high emissions
change in annual average temperatures, ºC