© Crown copyright Met · PDF fileRichard Betts, Martin Best, Pete Falloon, Simon...
Transcript of © Crown copyright Met · PDF fileRichard Betts, Martin Best, Pete Falloon, Simon...
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Climate change impactsAn overview of work at the Met Office Hadley CentrePete Falloon, UK-China INYS Workshop 27/02/2008
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Collaborators
Richard Betts, Martin Best, Pete Falloon, Simon Gosling1, Debbie Hemming, Matt Hills2, Tom Howard, Tomasz Kasikowsi, Neil Kaye, Jason Lowe, Mark McCarthy, Tom
Osborne2, Stephen Sitch, Sergey Venevsky3, Charlotte Wainwright2, Tim Wheeler2
Thanks to Olivier Boucher, Mat Collins, Peter Cox4, Chris Huntingford5, Chris Jones, Yadvinder Malhi6, Robert Nicholls7, Mike Sanderson, David Sexton, Mark Webb
1Kings College London, 2Walker Institute/Reading University, 3Leeds University, 4Exeter University, 5Centre for Ecology and Hydrology, 6Oxford University, 7Tyndall Centre/Southampton University
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Impacts assessments came as an “add-on” to climate modelling….
Human activity
Greenhouse climate change
ImpactsWater Food
Health Biodiversity etc…
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Human activity
Greenhouse climate change
ImpactsWater Food
Health Biodiversity etc…
But now we need a more robust and complete approach…
Other (local)
climate change)
e.g.: urban
heat islands
Other changes e.g.: air quality, land use
Interactions
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50% of the human population live on 3% of the Earths land surface
Figure from the UN department of Economic and Social Affairs
Night lights of the world from the US National Geographical Data Center
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Urban climate change has long been recognised
Night-time thermal image: 7-9-1991Courtesy of the ATSR project.
London up to 10oC warmer than rural area
•Increased storage of heat.
•Reduced evaporation.
•Anthropogenic heat release up to 1500Wm-2 (cf incident solar of 342Wm-2 or forcing of 4Wm-2 for doubled CO2)
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Projected increase in local temperature for a global average warming of 2 deg C
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Tem
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incr
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(deg
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Summer average Hottest day of the year
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Estimated percentage increase in mortality
• Based on summer average warming
• Doesn’t include adaptation
• Doesn’t include other health impacts (such as changes in air quality)
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Temperature change in cities due to doubling CO2 and tripling anthropogenic heat source
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Tem
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incr
ease
(°C
)
CO2 Increase Anthrop Increase
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Putting urban areas into the Regional climate model
T3
T2T1
T4
H1 H2 H3 H4
• MOSES2 land-surface tile-scheme
• Compare local warming in cities due to radiatively-forced climate change by doubled CO2 with that due to increased anthropogenic heat source
• Not possible for UKCIP08
Fractional coverage of urban areas in Europe
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Understanding uncertainties
Many sources of uncertainty in model projections…
Future emissions of greenhouse gases
Population, Technology, Political pressure
Incorrect, incomplete or missing description of key processes and feedbacks in the climate system
Representation of clouds, Feedback from land-use change
Differences in parameterisation
To understand these we use…
Ensembles of projections made from many different models
Plant productivity over Africa from the ‘QUMP’ perturbed parameter ensemble
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Future Plant Productivity changes & uncertaintieswith doubled CO2
Increases in plant productivity over most of tropics, temperate and boreal zones
Decreases in NE South America, southern Africa and Mediterranean basin
Uncertainties largest where changes biggest.
Usually uncertainties are smaller than average change
KgC/m2/yr
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Impacts of doubled-CO2 climate change on wheat production
Change in area suitable for spring wheat
Change in yield (%)
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Ozone Effects on Global Plant Productivity by 2100
Picture shows effects of high ozone concentration on plant growth
Future % changes in plant productivity due to higher ozone concentrations by 2100
% change in productivity
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Human health – modelled low level ozone
Yellow, orange & red colours highlight concentrations above 60ppb – the WHO 8 hr exposure dose guideline
Future ozone concentrations projected to rise above WHO guideline level in many (esp. highly populated) locations
Future low-level Ozone concentration – 2090s
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% of global population exposed to ozone above WHO guideline projected to increase significantly
Implications for world health policies
Courtesy of Michael Sanderson
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Future river flow + population changes (SRES A2 scenario)
% change in 2080s river flowPopulation change from 2000 to 2080(people per km2)
Less More
Less More
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Future changes in water stressbetween 1971-2000 and 2071-2100 (SRES A2)
Large areas show increasing water stress in 21st century
Increasedstress
Becomesstressed
NoNochangechange
ReducedReducedstressstress
StopsBeing stressed
Falkenmark Indicator: <1700m3 water per person per year = water stress
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How will carbon dioxide affect plants and global mean runoff ?
CO2 as greenhouse gas only
CO2 also affecting plant stomata
Less concern over drought?
More concern of flooding?
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Simulated burnt area
Observed burnt area
Simulated burnt area
Modelling fire in the global climate model
Fire risk and burnt area is simulated using temperature, humidity, windspeed and soil moisture
Simulated geographical and seasonal patterns of burnt area agree broadly with observations from satellite
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Number of extra people flooded by 2050s due to sea level rise and population change
Largest increases in number of people flooded (>2 million per year) expected in Bangladesh, south-east India and east coast of China
Thousands of people
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Storm surges
2080s minus present day A2 scenario
meters
Changes in 50-year storm surge height around UK
Water level up to 1.3m higher than present
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Human Health
Food and fibre resources
Water resources
River flooding
Coastal Flooding
Climate ChangeQuantifying Uncertainty
Urban Heat Islands
Air Quality
Land Use
Ecosystems & biodiversity