Transcript Slide 1
UN ECA - CILSS – ACMAD - IRI Conference on Reduction of vulnerability of West Africa to climate change Ouagadougou, January 24-27 2007 A climate scientist's perspective on recent environmental trends in the Sahel: a model for future change? Alessandra Giannini IRI for Climate and Society (IRI) The Earth Institute at Columbia University Outline – past, present and future of climate in the Sahel 1. oceanic forcing dominant in late 20th century droughts - what role for land-atmosphere interaction? 2. late 20th century response to anthropogenic forcings - roles of GreenHouse Gases and (sulfate) aerosols 3. why the uncertainty in projections of future change? - mechanisms of monsoon change under climate change r = 0.60 A. Giannini, R. Saravanan and P. Chang, 2003. Science, 302, 1027-1030 Also see e.g. Bader and Latif, 2003 (GRL); Lu and Delworth, 2005 (GRL);Tippett, 2006 (GRL) land-atmosphere interaction: is it a positive feedback? (soil moisture, vegetation, dust..., evaporation, cloud cover...) late 20th century surface temperature changes regression of NASA/NSIPP1 Sahel PC and sfc temp Giannini et al. 2003, 2005 NASA/GISS analysis of surface temp – linear trend 1950-2000 Hansen et al. 1999 (J. Geophys. Res.) IPCC 4AR: end 20th century – PreIndustrial sfc temp difference Biasutti and Giannini 2006 (GRL) IPCC 4AR simulations – late 20th century climate change 19 Coupled GCMs XX-PI Changes Biasutti and Giannini, GRL 2006 20th century Biasutti and Giannini, 2006 (GRL) Sahel climate change 21st century 19 Coupled GCM (IPCC 4AR): recent and future temperature changes A1B (end 21st) - end 20th end 20th - PreInd CONCLUSIONS (climate science) ● African climate variability and change are inextricably tied to variations and trends in the global climate system: -->> recent trends in the global oceans and in continental precipitation can in part be ascribed to anthropogenic forcings -->> drought in the Sahel was forced by a warming of the oceans, in no negligible part due to GHG and aerosol forcing “Farmers freed of blame for Sahel drought” in http://www.scidev.net/ CONCLUSIONS (climate science informing policy) ● Climate change is already here the recent climate shift in the Sahel is a prime example of potential changes to come, as the global climate system responds to anthropogenic forcings -->> regional institutions/CILSS have an opportunity to take advantage of the lessons learned from managing the climate shift of the last ~30 years -->> harmonization of desertification and climate change issues is overdue! CONCLUSIONS (climate science informing practice - climate risk management) collaborate on climate science ● improve (two-way) communication ● -->> between climate scientists and policymakers -->> between climate scientists and stakeholders in sectors vulnerable to climate http://iridl.ldeo.columbia.edu/index.html http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php West Africa: 0-20N, 20W-20E Eastern eq Africa: 10S-10N, 20-50E Southern Africa: 25-10S, 20-40E West Africa: 0-20N, 20W-20E Eastern eq Africa: 10S-10N, 20-50E Southern Africa: 25-10S, 20-40E Courtesy of Todd Mitchell, UW/JISAO Giannini et al., 2005 (Clim. Dyn.) The relative roles of Atlantic, Indian and Pacific SSTs Lu and Delworth, 2005 (Geophys. Res. Lett.) GFDL CM2.0 Held et al., PNAS 2005 GMAO(NSIPP1) NCAR CAM3 surface air temperature (minus global mean) precipitation Haarsma et al., GRL 2005 2050-2080 minus 1950-1980