Harmattan, Saharan heat low, and West African monsoon circulation: modulations on the Saharan dust outflow towards the North Atlantic

The outflow of dust from the northern African continent towards the North Atlantic is stimulated by the atmospheric circulation over North Africa, which modulates the spatio-temporal distribution of dust source activation and consequently the entrainment of mineral dust into the boundary layer,...

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Bibliographic Details
Main Authors: K. Schepanski, B. Heinold, I. Tegen
Format: Article
Language:English
Published: Copernicus Publications 2017-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/17/10223/2017/acp-17-10223-2017.pdf