Interpretation of climate change using maps of climate analogues in the DRIAS climate services project Julien Lémond 1-2, S. Planton 1, M. Ha-Duong 3,

Slides:



Advertisements
Similar presentations
COSMO User Seminar 2012 Offenbach, 8 March 2012
Advertisements

© UKCIP 2006 UKCIP08 What to expect from the next set of climate change scenarios Richard Lamb UK Climate Impacts Programme.
OSE meeting GODAE, Toulouse 4-5 June 2009 Interest of assimilating future Sea Surface Salinity measurements.
Climate changes in Southern Africa; downscaling future (IPCC) projections Olivier Crespo Thanks to M. Tadross Climate Systems Analysis Group University.
Scaling Laws, Scale Invariance, and Climate Prediction
© Crown copyright Met Office Climate Projections over Mainland China under SRES A1B and RCP4.5 Using PRECIS 2.0 Changgui Wang, Richard Jones.
Earth Science & Climate Change
Consistency of recently observed trends over the Baltic Sea basin with climate change projections 7th Study Conference on BALTEX June 2013, Sweden.
Downscaling and Uncertainty
Progress in Downscaling Climate Change Scenarios in Idaho Brandon C. Moore.
Detection of Human Influence on Extreme Precipitation 11 th IMSC, Edinburgh, July 2010 Seung-Ki Min 1, Xuebin Zhang 1, Francis Zwiers 1 & Gabi Hegerl.
Past and future changes in temperature extremes in Australia: a global context Workshop on metrics and methodologies of estimation of extreme climate events,
Federal Departement of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Present-day interannual variability of surface climate.
Projection of future climate change conditions using IPCC simulations, neural networks and Bayesian statistics. Temperature and Precipitation mean state.
Use of the Spatial Analogy in Climate Change Research Horváth, Levente – Gaál, Márta – Erdélyi, Éva Debrecen 2006.
Global Climate Change: The Heart of the Matter. What we can see (observations) What is causing it (causes and evidence) What can happen (projections)
Linking probabilistic climate scenarios with downscaling methods for impact studies Dr Hayley Fowler School of Civil Engineering and Geosciences University.
NCPP – needs, process components, structure of scientific climate impacts study approach, etc.
Page 1GMES - ENSEMBLES 2008 ENSEMBLES. Page 2GMES - ENSEMBLES 2008 The ENSEMBLES Project  Began 4 years ago, will end in December 2009  Supported by.
Climate Forecasting Unit Second Ph’d training talk Prediction of climate extreme events at seasonal and decadal time scale Aida Pintó Biescas.
Update on EURO-CORDEX and MED-CORDEX Filippo Giorgi Abdus Salam ICTP CORDEX-SAT1, Trieste, May, 2014.
Climate Forecasting Unit Prediction of climate extreme events at seasonal and decadal time scale Aida Pintó Biescas.
© Crown copyright Met Office Climate Projections for West Africa Andrew Hartley, Met Office: PARCC national workshop on climate information and species.
The Eta Regional Climate Model: Model Development and Its Sensitivity in NAMAP Experiments to Gulf of California Sea Surface Temperature Treatment Rongqian.
Zhang Mingwei 1, Deng Hui 2,3, Ren Jianqiang 2,3, Fan Jinlong 1, Li Guicai 1, Chen Zhongxin 2,3 1. National satellite Meteorological Center, Beijing, China.
Recent developments in seasonal forecasting at French NMS Michel Déqué Météo-France, Toulouse.
Initiatives toward Climate Services in France and in the European Communities C. Déandreis (CNRS/IPSL); M. Plieger and W. Som de Cerff (KNMI); Ph. Dandin,
Assessing trends in observed and modelled climate extremes over Australia in relation to future projections Extremes in a changing climate, KNMI, The Netherlands,
Gridding Daily Climate Variables for use in ENSEMBLES Malcolm Haylock, Climatic Research Unit Nynke Hofstra, Mark New, Phil Jones.
The Euro- and City-Delta model intercomparison exercises P. Thunis, K. Cuvelier Joint Research Centre, Ispra.
DRIAS Project: providing Regional Climate Informations over France Julien Lémond 1-4, Ph. Dandin 1, S. Planton 4, R. Vautard 3, C. Pagé 2, M. Déqué 4,
CERFACS: Christian Pagé Laurent Terray Météo-France: Philippe Dandin Pascale Delecluse Serge Planton Jean-Marc Moisselin Maryvonne Kerdoncuff High resolution.
Jana Sillmann Max Planck Institute for Meteorology, Hamburg
Numerical modelling of possible catastrophic climate changes E.V. Volodin, N. A. Diansky, V.Ya. Galin, V.P. Dymnikov, V.N. Lykossov Institute of Numerical.
Downscaling and its limitation on climate change impact assessments Sepo Hachigonta University of Cape Town South Africa “Building Food Security in the.
Modelling of climate and climate change Čedo Branković Croatian Meteorological and Hydrological Service (DHMZ) Zagreb
© Crown copyright Met Office Providing High-Resolution Regional Climates for Vulnerability Assessment and Adaptation Planning Joseph Intsiful, African.
Adaptation Baselines Through V&A Assessments Prof. Helmy Eid Climate Change Experts (SWERI) ARC Egypt Material for : Montreal Workshop 2001.
Reducing Canada's vulnerability to climate change - ESS J28 Earth Science for National Action on Climate Change Canada Water Accounts AET estimates for.
Building Asian Climate Change Scenarios by Multi-Regional Climate Models Ensemble S. Wang, D. Lee, J. McGregor, W. Gutowski, K. Dairaku, X. Gao, S. Hong,
The Tyndall Centre comprises nine UK research institutions. It is funded by three Research Councils - NERC, EPSRC and ESRC – and receives additional support.
Components of the Global Climate Change Process IPCC AR4.
Federal Departement of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Revisiting Swiss temperature trends * Paulo.
The Tyndall Centre comprises nine UK research institutions. It is funded by three Research Councils - NERC, EPSRC and ESRC – and receives additional support.
Climate information for the wind energy industry in the Mediterranean Region: from ENSEMBLES to MED- CORDEX Alessandro Dell'Aquila, ENEA Sandro Calmanti,
The European Heat Wave of 2003: A Modeling Study Using the NSIPP-1 AGCM. Global Modeling and Assimilation Office, NASA/GSFC Philip Pegion (1), Siegfried.
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
Feng Zhang and Aris Georgakakos School of Civil and Environmental Engineering, Georgia Institute of Technology Sample of Chart Subheading Goes Here Comparing.
Simulated and Observed Atmospheric Circulation Patterns Associated with Extreme Temperature Days over North America Paul C. Loikith California Institute.
Statistical Post Processing - Using Reforecast to Improve GEFS Forecast Yuejian Zhu Hong Guan and Bo Cui ECM/NCEP/NWS Dec. 3 rd 2013 Acknowledgements:
Production of a multi-model, convective- scale superensemble over western Europe as part of the SESAR project EMS Annual Conference, Sept. 13 th, 2013.
© Crown copyright Met Office Downscaling ability of the HadRM3P model over North America Wilfran Moufouma-Okia and Richard Jones.
Copernicus Observations Requirements Workshop, Reading Requirements from agriculture applications Nadine Gobron On behalf Andrea Toreti & MARS colleagues.
The ENSEMBLES high- resolution gridded daily observed dataset Malcolm Haylock, Phil Jones, Climatic Research Unit, UK WP5.1 team: KNMI, MeteoSwiss, Oxford.
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 Extreme Climatic and atmospheric.
1 Implications of trends in the Asian monsoon for population migrations Dr. D. B. Stephenson, Dr. E. Black, Prof. J.M. Slingo Department of Meteorology,
Consistency of recent climate change and expectation as depicted by scenarios over the Baltic Sea Catchment and the Mediterranean region Hans von Storch,
1/39 Seasonal Prediction of Asian Monsoon: Predictability Issues and Limitations Arun Kumar Climate Prediction Center
1 CL2.16 Urban climate, urban heat island and urban biometeorology H How to obtain atmospheric forcing fields for Surface Energy Balance models in climatic.
Dynamics of the African Heat Low on climate scale R. Roehrig, F. Chauvin, J.-P. Lafore Météo-France, CNRM-GAME ENSEMBLES RT3 Working Meeting 10 February.
Can recently observed precipitation trends over the Mediterranean area be explained by climate change projections? Armineh Barkhordarian1, Hans von Storch1,2.
A BAYESIAN ENSEMBLE METHOD FOR CLIMATE CHANGE PROJECTION
Climate Change in Scotland / UK / N. Europe
On HRM3 (a.k.a. HadRM3P, a.k.a. PRECIS) North American simulations
The C3S project UrbanSIS - 1km resolution ECVs and impact indicators over European cities focusing on health and infrastructure Lars Gidhagen, Jorge H.
Hydrologic response of Pacific Northwest Rivers to climate change
University of Washington Center for Science in the Earth System
1 GFDL-NOAA, 2 Princeton University, 3 BSC, 4 Cerfacs, 5 UCAR
Relative impacts of mitigation, temperature, and precipitation on 21st-century megadrought risk in the American Southwest by Toby R. Ault, Justin S. Mankin,
Presentation transcript:

Interpretation of climate change using maps of climate analogues in the DRIAS climate services project Julien Lémond 1-2, S. Planton 1, M. Ha-Duong 3, Ph. Dandin 2 1 CNRM-GAME, Météo-France, CNRS, Toulouse, France 2 Direction of Climatology, Météo-France, Toulouse, France 3 CIRED, Paris, France 11th EMS / 10th ECAM Berlin, 13 September 2011

 Global warming is unequivocal (IPCC, 2007) –Need for adaptation and mitigation  Why an approach by analogy? –Analogy is an efficient way to communicate on complex issues –Results could be used by people with a no scientific background  Climate analogues consist in seaching in the current climate, regions with similar climate than expected in the future for a considered city (c.f. Hallegate et al.,2007; Kopf et al. 2008)  Why a study on climate around urban areas? –Most of the european populations live in a city –Strong impact of an increase of temperature in these areas (e.g. heat wave in 2003 or 2006)  This study is lead in frame of the project DRIAS, which aims at facilitating the access to climate scenarios information Context – Rationale

Presentation Outline  1°) Context - Rationale  2°) Data and Method  3°) Main Results  4°) Conclusion

Data: RCMs from ENSEMBLES project  Main issues: –Taking uncertainties into account: need of several climate models –Necessity of high spatial resolution: need of regional climate models The climate projections used in this study have been produced for the European project ENSEMBLES InstitutionRCMDriving GCMRCM References C4lRCAHadCM3Q16Kjellström et al. (2005) CNRMALADINARPEGE_RM5.1Radu et al. (2008) DMIHIRHAMECHAM5-r3Christensen et al. (1996) DMIHIRHAMARPEGEChristensen et al. (1996) ETHZCLMHadCM3Q0Böhm et al. (2006) ICTPRegCMECHAM5-r3Giorgi and Mearns (1999) KNMIRACMOECHAM5-r3Lenderik et al. (2003) MPIREMOECHAM5-r3Jacob (2001) SHMIRCAECHAM5-r3Kjellström et al. (2005) Regional Climate Model and Driving General Climate Model used in the study:

 Parameters used: –Surface temperature –Total Precipitation  Resolutions: –Spatial: 25 km –Temporal: daily  Time periods defined: –Reference: –Near projection: –Middle projection: –Far projection:  Seasons defined: –Summer: June-July-August (JJA) –Winter: December-January-Febuary (DJF) Parameters, resolutions and time periods

 Spatial interpolation (bicubic interpolation)  Ocean-Land mask  Quantile-Quantile correction (Déqué, 2007) Pre-processing Black line: raw output model PDF Dashed black line: observations E-OBS PDF Red line: corrected model PDF Example of correction for summer temperature, for a grid-point (data from CNRM model) Observations used are from the ENSEMBLES daily gridded observational dataset (called E-OBS; V3; Haylock et al., 2008) temperature density

The 2-Dimensional Kolmogorov-Smirnov test (Peacock, 1983; Kopf et al., 2008) A Statistical method used to computed analogues Illustration of the 2D KS-test for climatic samples (From Kopf et al., 2008) 1)Selection of future projections of seasonal temperature and precipitation of the closest grid- point for the studied city (e.g. Paris) 2)Statistical measure of climatic similarity with reference climate, for all the grid-point of the European domain studied

Presentation Outline  1°) Context - Rationale  2°) Data and Method  3°) Main Results  4°) Conclusion

Inter-model spread (1/2) Shade key: 1 -> Bad analogues 0 -> Good analogues  Results for : –Paris, Winter (DJF), Near Projection ( ) –9 models and multimodels ensemble

Inter-model spread (2/2) Shade key: 1 -> Bad analogues 0 -> Good analogues  Results for : –Paris, Summer (JJA), Near Projection ( ) –9 models and multimodels ensemble

Climate analogues for Paris from multi-models ensemble WinterSummer Shade key: 1 -> Bad analogues 0 -> Good analogues

WinterSummer Shade key: 1 -> Bad analogues 0 -> Good analogues Climate analogues for Berlin from multi-models ensemble

trajectories of the best analogues Paris Berlin LondonMadrid Best analogues for time periods: H1: H2: H3: Blue: Winter (DJF) Red: Summer (JJA)

Conclusion  This study’s aims has been to develop, in frame of the project DRIAS, a climate product easily useable by people involved in impact and adaptation issues  Following Hallegate et al. (2007) and Kopf et al. (2008), analogue approach has been used. That consist in seaching in the current climate, regions with similar climate than expected in the future for a considered city  Maps of climate analogues and trajectories of best analogues have been computed using a 2D KS test and a multi-models ensemble (9 RCMs from the EMSEMBLES project)  A seasonal study has been done on corrected data  More sophistical definition of best analogue could be explored