Effects of Saharan dusts on weather and climate

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Effects of Saharan dusts on weather and climate over the Atlantic: How Nature foiled

Effects of Saharan dusts on weather and climate over the Atlantic: How Nature foiled the 2006 hurricane forecasts William K. M. Lau NASA/GSFC Laboratory for Atmospheres Co-author: K. M. Kim/GEST

Effects of Saharan dusts on weather and climate over the Atlantic • Annual emission

Effects of Saharan dusts on weather and climate over the Atlantic • Annual emission of Saharan dust is estimated to be 4 billion tons • Increased Saharan dust outbreak since the 1970’s, associated with the prolonged drought in Sahel and increased dust storm over the Sahara desert Possible weather and climate impacts: • SAL dry air may suppress tropical cyclogenesis, and/or hurricane formation • Microphysics effects: suppress warm rain; increase ice-nucleation and deep convection • • Solar Dimming Effect “ Elevated Heat Pump” Effect MODIS Images

How did nature foil the 2006 hurricane forecasts? 2005 15 H, 12 TS, 2

How did nature foil the 2006 hurricane forecasts? 2005 15 H, 12 TS, 2 TD, 1 STS, 1 STD 2006 5 H, 4 TS

El Nino-SST effect Dust-SST “Solar Dimming” effect Dust appears to be the primary cause

El Nino-SST effect Dust-SST “Solar Dimming” effect Dust appears to be the primary cause for SST cooling in the MDR; El Nino is associated with reduced SST (and increased vertical shear) in the eastern equatorial Atlantic, suppresses cyclogensis

More dust means lesser number of days of tropical cyclones

More dust means lesser number of days of tropical cyclones

Correlations of HC/TS statistics with a) Barbados dust and b) El Nino SST, 1980

Correlations of HC/TS statistics with a) Barbados dust and b) El Nino SST, 1980 -2007 • TS = sustained wind speed > 34 knts (17 m/s) HC = sustained wind speed >64 knts (33 m/s)

The “Elevated Heat Pump” effect : fv. GCM simulation of radiative Effect on circulation

The “Elevated Heat Pump” effect : fv. GCM simulation of radiative Effect on circulation and climate of the West African region Caribbean Africa

Gulf of Guinea Africa

Gulf of Guinea Africa

Short wave flux = -30. 4 Wm-2 Longwave flux = 5. 9 Wm-2 Sensible

Short wave flux = -30. 4 Wm-2 Longwave flux = 5. 9 Wm-2 Sensible heat flux = 2. 1 Wm-2 Latent heat flux = 8. 6 Wm-2 Net surface flux = -14. 1 Wm-2 Estimate of anomalous (aerosol+ water cycle feedback) surface energy flux over the N. Atlantic/Caribbean region

Anomalous Overturning Circulation induced by “Elevated Heat Pump” effect for WAM increased upper level

Anomalous Overturning Circulation induced by “Elevated Heat Pump” effect for WAM increased upper level clouds reduced upper level clouds induced subsidence suppresses convection increased low level clouds increased moisture influx reduced SW Caribbean Region cools ocean reduced SW cools land Africa dust source

West Africa East Atlantic Caribbean

West Africa East Atlantic Caribbean