Highlights of PRUDENCE Results on future extreme events simulated by Regional Climate Models
European regional climate change and the PRUDENCE project
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Transcript of European regional climate change and the PRUDENCE project
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European regional climate European regional climate change and the PRUDENCE change and the PRUDENCE
projectproject
Ole Bøssing ChristensenDMI
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IPCC AR4 CH. 11 structure IPCC AR4 CH. 11 structure Jens H. Christensen (CLA)Jens H. Christensen (CLA)
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Chapter 11 structure : Regional Climate ProjectionsLength:60 printed pages including all refs and figures, excl. FAQCLAs: Christensen and HewitsonLAs: Busuioc, Chen, Gao, Held, Jones, Kwon, Laprise, Magana, Mearns, Menendez, Räisänen, Rinke, Kumar, Sarr, Whetton
Executive summary (1-2 pages)11.1 Introduction (3 pages)
11.1.1 The importance of regional projections11.1.2 Summary of the TAR11.1.3 Developments since the TAR
11.2 Assessment of Methods11.2.1 Generating regional information (5 pages)
11.2.1.1 AOGCM results11.2.1.2 High resolution AGCMs11.2.1.3 Nested RCMs11.2.1.4 Statistical downscaling11.2.1.5 Pattern scaling of climate model simulations11.2.1.6 Other methods11.2.1.7 Inter-comparison of methods
11.2.2 Quantifying uncertainties (3-4 pages)11.2.2.1 Sources of regional uncertainty11.2.2.2 Methodological developments
11.3 Regional Projections (30 pages)Details on following slides
11.4 Conclusions and discussion (1 page)
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11.3 Regional Projections (30 pages)11.3.1 Introduction to regions and relationship to WGII regions (1 page) (Any sub-regions listed below may be further sub-divided if authors feel this is appropriate)(Length: nominally 3-4 pages each)11.3.2 Africa
Sahelian AfricaHorn of Africa / Arabian peninsulaEquatorial AfricaSouthern Africa
11.3.3 Mediterranean and EuropeMediterraneanCentral and northern Europe
11.3.4 AsiaCentral AsiaSouth AsiaEast AsiaSouth east Asia / Maritime continent
11.3.5 North America North America
11.3.6 Latin AmericaCentral America / CaribbeanNorthern South AmericaSouthern South America
11.3.7 Australia and New ZealandAustralia/New Zealand
11.3.8 PolarArcticAntarctic
11.3.9 Small Islands
Chapter 11 structure : Regional Climate Projections
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Chapter 11 structure : Regional Climate Projections
BOX 11.1: Summary of AOGCM regional projections (2 pages) Consistent method across regions, & to include uncertainty
Probabilistic statements based on AOGCMs, in coordination with Ch 10
BOX 11.2: Common aspects of small scale climate change : High altitude (1 page)
BOX 11.3: Common aspects of small scale climate change : Coastal (1 page)
Table 11.1: Extremes (1 page)Summary table in collaboration with Ch 3,4,5,9,10 & WGII
FAQ
Proposed FAQ: a) Does this report say anything about what will happen in my back
yard?b) Will the weather become more extreme?c) How can I use regional information that is uncertain?
(Why are regional projections useful?) d) What’s downscaling?e) What’s wrong with extending recent regional trends?
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IPCC WG1 IPCC WG1 scheduleschedule
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PRUDENCE participantsPRUDENCE participants1. Danish Meteorological Institute, Copenhagen, DK2. CINECA, Bologna, IT3. Météo-France/CNRM, Toulouse, FRA4. Deutsches Zentrum für Luft- und Raumfahrt e.V., Weßling, GER5. Hadley Centre for Climate Prediction and Research, Met Office, Bracknell, UK6. Climate Research ETH (Eidsgenössische Technische Hochschule), Zürich, CH7. GKSS Research Center (Institute for Coastal Research), Geesthacht, GER8. Max-Planck-Institut für Meteorologie, Hamburg, GER9. Swedish Meteorological and Hydrological Institute, Rossby Centre, Norrköping, SWE10. Universidad Complutense, Madrid, SP11. Universidad Politecnica, Madrid, SP12. International Centre for Theoretical Physics, Trieste, IT13. Danish Institute of Agricultural Sciences, Foulum, DK14. Risø National Laboratory, System Analysis Dept., DK15. University of Fribourg, CH16. Finnish Environmental Institute, Helsinki, FIN17. University of Reading, UK18. University of Lund, SWE19. Centre International de Recherche sur l’Environnement et le Développement, SMASH, Paris, FRA20. Climate Research Unit, University of East Anglia, UK21. Finnish Meteorological Institute, Associated to FEI (No. 16), FINA. Norwegian Meteorological Institute, Blindern, NOB. Royal Dutch Meteorological Institute, De Bilt, NLC. UQAM, Montreal, CAND. CSIRO, Victoria, AUSE. Czech Republic, Israel, Greece, Belgium, Slovakia………………..F. Munich-Re, Electricité de France, Elforsk, Hamburg Institute of International Economics,
Uni-Münster, DG-Research, STARDEX, MICE
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PRUDENCE objectivesPRUDENCE objectives A series of high resolution climate change scenarios for 2071-2100 for Europe
Characterize level of confidence and variability related to model formulations and climate natural/internal variability
Assess the uncertainty in European regional scenarios resulting from model formulation
Quantitatively assess the risks arising from changes in regional climate over Europe, and estimate changes in extremes like heat waves, flooding and wind storms, by providing a robust estimation of the likelihood and magnitude of the changes
Demonstrate the value of the wide-ranging scenarios by applying them to impacts models focusing on effects on adaptation and mitigation strategies
Assess socio-economic and policy related decisions for which such improved scenarios could be beneficial
Disseminate the results of PRUDENCE widely …
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150km globalatmospheric
GCM
12-50km RCMfor relevant region
Coupled GCM (300km atmosphere)
A modelling system for detailed regional scenarios –
the PRUDENCE method
Observed SST/sea-ice
SST/sea-ice change from coupled GCM
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Quasi-ensemble probabilitiesQuasi-ensemble probabilities
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Precipitation change – Precipitation change – sources of uncertaintysources of uncertainty
95%-confidence: internal variability
C. Frei, ETH
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OBS: Slightly different values since the changes in precipitation have been scaled to a 3 K change of the global mean temperature
Precipitation change – Precipitation change – sources of uncertaintysources of uncertainty95%-confidence: GCM formulation, RCM formulation, internal variability
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Probabilistic precipitation Probabilistic precipitation changechange
Sensitivity x signal
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Variability sources in sub-areasVariability sources in sub-areas
3 France
1 British Isles2 Iberian peninsula
4 Central Europe5 Scandinavia6 Alps7 Mediterranean8 Eastern Europe
M. Déqué, Météo-France
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Temperature change – Temperature change – sources of uncertaintysources of uncertainty
DJF
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Depends on driving model
Also on RCM and scenario
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Precipitation change – Precipitation change – sources of uncertaintysources of uncertainty
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Driving GCM and RCM
RCM quite important
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Baltic water balanceBaltic water balance
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9 RCMs (2 GCMs) 9 RCMs (2 GCMs) ~~50 km 50 km - 2 RCMs - 2 RCMs ~~25 km A225 km A2
-- 3 RCMs 3 RCMs ~~50 km50 km B2B2
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PRUDENCE work on extremesPRUDENCE work on extremes
Better understanding of how European weather and climate extremes are likely to change:
Heat waves
Precipitation – heavy and low
Wind storms and storm surges
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Precipitation extremesPrecipitation extremes
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Changes in HIRHAM 5-year return levelsChanges in HIRHAM 5-year return levels5-day Winter precipitation Summer 1-day precipitation
Increases over Europe except for decreases in south in summer
HIRHAM
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Christensen & Christensen, Nature (2003)
Sensitivity due to GCM and RCM resolutionSensitivity due to GCM and RCM resolution
ECHAM HC 50km HC 25km
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JAS precipitation [mm/day] JAS precipitation [mm/day] Resolution 50kmResolution 50km
90% wd 95% wd
99% wd 99.9% wd
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90% wd 95% wd
99% wd 99.9% wd
JAS precipitation [mm/day] JAS precipitation [mm/day] Resolution 25kmResolution 25km
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90% wd 95% wd
99% wd 99.9% wd
JAS precipitation [mm/day] JAS precipitation [mm/day] Resolution 12kmResolution 12km
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Wind extremesWind extremes
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% change in 90% change in 90thth percentile of 10-metre wind speed percentile of 10-metre wind speed
Increased wind speed intensity in core of Europe north of Alps
RCAO
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A2 changes in max winter surge heightsA2 changes in max winter surge heights
HIRHAM
Largest change of 0.3 metres on coasts near German bightChanges (meters) in max surge heights from HadAM3H / HIRHAM.
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ConclusionsConclusionsWarming of near-surface temperatures•DJF: west/east gradient with strongest warming in the east•JJA: north/south gradient with strongest warming in the south
Changes in precipitation•DJF: mainly due to driving GCM but also due to RCM•JJA: dryer conditions in all but northern Europe
Large ensemble of simulations allows for the generation of probabilistic regional climate scenarios
Uncertainty of temperature changes•DJF: mainly due to driving GCM•JJA: also due to RCM and scenario
Uncertainty of changes in precipitation•DJF: mainly due to driving GCM but also due to RCM•JJA: to a large extent due to RCM
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ConclusionsConclusions•Significant changes of the discharge into the Baltic
•Increased magnitude due to enhanced winter precipitation
•Earlier peak due to earlier snow melt
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ConclusionsConclusions
• Heat waves – increased frequency, intensity, and duration of summer heat waves
• Increase in interannual variability of temperature –Summer 2003 could become more likely
• Heavy precipitation – general increase except over S. Europe in summer. Central Europe will have less rainy days, but probably larger intensities
• Wind storms –increased intensity and frequency of high wind speed events in winter
• Storm surges –increase in maximum storm surge level of up to 0.3 metres especially near the German Bight.
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Near-surface temperature Near-surface temperature change - DJFchange - DJF
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Near-surface temperature Near-surface temperature change - JJAchange - JJA