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The Impacts of the Indian Ocean warming trend on African Climate. Dan Hodson and Rowan Sutton NCAS Centre for Global Atmospheric Modelling Department of Meteorology University of Reading
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Outline Observations. Experiments I –Atmosphere model forced with: Historical Observed Sea Surface Temperatures. 1°C Anomaly in the Indian Ocean Indian Ocean Temperature Trend Experiments II –Atmosphere model force with Observed Indian Ocean warming Trend Results Conclusions and Caveats
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Observations
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Hoerling et al. J. Climate 2006 1950-1999 Trend in Rainfall
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Experiments I
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AGCM forced with Observed SSTs
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AGCM Forced with Obs SSTs 1950-1999 Hoerling et al. J. Climate 2006 FMA
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AGCM Forced with Obs SSTs 1950-1999 Hoerling et al. J. Climate 2006 JAS
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AGCM forced with 1°C Indian Ocean
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+1°C
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AGCM Forced with 1C Indian Ocean Anomaly
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Indian Ocean Temperature Trend
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Indian Ocean SST Trend C
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Indian Ocean SST trend Annual mean SST trend 1951-1990 C/year 0.02 -0.02
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Atmosphere model force with Observed Indian Ocean warming Trend
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Jan May Sept SST Anomalies
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Indian Ocean SST Trend C IOP ION
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Experiment Five AGCMs –Arpege –CAM3 –Echam5 –GAM (IAP) –HadAM3 Indian Ocean Positive (IOP) Indian Ocean Negative (ION)
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Results
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FMA Vertical velocityRainfallSurface Temperature ARP CAM ECH GAM HAD
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JAS Vertical velocityRainfallSurface Temperature ARP CAM ECH GAM HAD
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Caveats?
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Observed MSLP trends Copsey et al GRL 2006
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MSLP Trends
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Conclusions AGCMs forced with warm Indian Ocean capture some of the trends in African rainfall (both FMA and JAS). Trends associated with changes in subsidence/ changes in Walker Circulation. Can we use AGCMs to model past changes in this way?
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Vertical Structure JAS
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Vertical Structure FMA
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Station rainfall trends 1950-1999 (JAS/FMA)
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