Effects of Saharan dusts on weather and climate
- Slides: 14
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 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 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 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
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 and climate of the West African region Caribbean Africa
Gulf of Guinea Africa
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 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
- Great zimbabwe spice chart
- Galactic city model
- Trans saharan trade route map
- Trade routes in the 1500s
- Sub saharan africa physical features
- Trans saharan trade
- African city model
- Sub saharan africa landforms
- Trans saharan trade route
- Sub-saharan africa
- Sub saharan africa ap world history
- Climate change 2014 mitigation of climate change
- How does wind affect weather and climate
- Clim 101
- How do prevailing winds affect climate