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Dynamics of the West African Monsoon Jump
2007
Journal of Climate
The observed abrupt latitudinal shift of maximum precipitation from the Guinean coast into the Sahel region in June, known as the West African monsoon jump, is studied using a regional climate model. Moisture, momentum, and energy budget analyses are used to better understand the physical processes that lead to the jump. Because of the distribution of albedo and surface moisture, a sensible heating maximum is in place over the Sahel region throughout the spring. In early May, this sensible
doi:10.1175/2007jcli1533.1
fatcat:bscgpxl7pvckfhy2e5piaifwku