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Download Climate change scenarios for West Africa - START
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Assessing Global and Regional climate change scenarios for West Africa GOALS 1) using outputs from GCMs to drive a regional climate model at the lateral boundaries at 6 or 12-hour periods. - Because of the relatively sharp vegetation gradients and important orographic features the regional model may provide a different solution of future climate change relative to GCMs. - The regional climate model run at 60 km and the output can be used as input to statistical models for further downscaling or used as input into hydrologic, economic or agricultural models. 2) Capacity building in West Africa - regional and global climate modelling - analysis of climate processes BACKGROUND - Provide requisite climate change scenarios for Mali needed to undertake vulnerability studies Methods Statistical &empirical Downscaling of GCM outputs Socio-economic scenarios - MSL - GW MAGICC SCENGEN - Spatial patterns of standardized GCM outputs interpolation of changes fields to locations of interest from nearby GCM grid boxes 1) direct interpolation 2) regressing grid box data using coefficient deduced from observations at subscale locations Which GCM to use? Horizon 2025 15 10 Delta_P (% ) 5 0 0 0,5 1 1,5 -5 2 2,5 - above normal - normal - below normal -10 -15 -20 Delta_T (°C) Scatterplot of Temperature and Precipitation projections showing 3 categories of outpouts (2025) Delta_P (%) Taux de variation de la pluviométrie par rapport à la normale 1961-90 à Bougouni 30 20 10 2025 2050 2075 2100 0 -10 J F M A M J J A S O N D -20 -30 -40 -50 month Projections of mean monthly rainfall at one location of the study area (in Mali CC study) West African context - West Africa experienced downward reduction in rain amounts over the last three decades - factors potentially responsible for reduced rain amounts: land-use change, Atlantic and global SST anomalies, inter-hemispheric SST trends, lower and upper troposphere wind anomalies and anthropogenic greenhouse forcing - Changes in the regional climate of West Africa remain uncertain, especially with respect to rain, because much of the rain that falls is associated with mesoscale convective systems such as squall lines and mesoscale convective complexes (MCCs). Moreover these systems are associated with synoptic-scale easterly waves, which are responsible for tropical cyclones in the Atlantic Basin. OBJECTIVES (a) assess GCM and regional climate model simulations for present and future climate states in order to examine the processes that bring about new climate states. Evaluate GCM scenarios based on given emission scenarios during the 20th and 21st century, identifying strengths and weaknesses of GCM simulations on seasonal, annual and decadal time-scales for West Africa. (b) Determine whether these changes are realistic given our current understanding of the West African Climate system. (c) Provide model outputs to other disciplines so that they can examine how potential changes in climate might affect key sectors on national and regional scales in West Africa. TROPICAL TROPOSPHERIC DYNAMICS ALREADY DEVELOPED GCM (CCM/NCAR) DEVELOPMENT OF A MESOSCALE MODEL FOR TROPICAL SYSTEMS RUNNING A REGIONAL CLIMATE MODEL (MM5 v3) ADAM Aerosol PROJECT Input A REALISTIC WESTERN AFRICA REGIONAL CLIMATE MODEL THAT MAY, FOR THE FIRST TIME, ADDRESS ISSUES LIKE: Effects of climate change on water resources Effects of climate change on agriculture Effects of climate change on health-related Effects of climate change on energy sources LOCAL EFFECTS METHODOLOGY GCM SIMULATION - Evaluation of mean states (current climate) - Evaluation of model variability (current climate) - Evaluation of changes in the mean state due to anthropogenic Ghg between 20th and 21 sh century RCM SIMULATION - MM5 v3 modified & land surface package (LSX) & Genesis (surface hydrology and energy budget) - RCM driven at lateral boundaries by 6 and 12h data from CCSM and emission scenario (SRES A1, ….) Visualization - outputs on ncdf formats INVESTIGATORS Principal Investigator Amadou Gaye, Senegal Laboratory of Atmospheric Physics, Dakar University Co-investigators: Adamou Garba, Niger Affiliation: EAMAC School of Meteorology, Niamey, Niger Andre Kamga , Cameroun Affiliation: Applied Physics Research Center (CEPAMOQ)/ Environment and pollution Program p.o.box 24157 Douala - Cameroon. Arona Diedhiou, Senegal Affiliation: LTHE, IRD Grenoble France Akintayo Adedoyin, Nigeria Affiliation: University of Botswana Abdoulaye Sarr, SENEGAL Affiliation: ASECNA Dakar & LPASF Dakar University Dakar Gregory S. Jenkins, USA Affiliation Department of Meteorology, Penn State University Continuing work on RCM and assessment of scenarios