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A Revised View of the West African Monsoon and Its Implications for Interannual and Interdecadal Variability

 

 

Sharon E. Nicholson

Department of Meteorology

Florida State University

                                                                         

 

    The classic view of the West African monsoon was created by colonial meteorologists active in forecasting in the 1950s.  The basic elements were that rainfall was linked to the Inter-tropical Convergence Zone but convection was substantially equatorward of the ITCZ because a certain depth of the moist monsoon layer was required to sustain deep convective clouds. A new analysis based on NCEP Reanalysis Data suggests a substantially different picture in which the ITCZ plays little role in the precipitation process and the major players are the African Easterly Jet, the Tropical Easterly Jet and a low-level off-equatorial westerly jet.  In most years the ITCZ is completely decoupled from these features.  In this study, factors affecting both the intensity and location of the rains over West Africa are considered.  Critical factors are the pressure gradient over the equatorial Atlantic, which influences the low-level westerly jet, and the instabilities and wave dynamics determined by the intensity of the TEJ and the location of the AEJ. 

These factors explain both interannual and interdecadal variability.
 

 

 

Thursday, 30 March 2006, 3:30 PM

Refreshments 3:15 PM

NCAR-Foothills Laboratory

3450 Mitchell Lane

Bldg 2 Auditorium (Rm. 1022)