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Journal Article: BibTeX citation key:  Cuesta2009b
Cuesta, J., Marsham, J. H., Parker, D. J. & Flamant, C. (2009) Dynamical mechanisms controlling the vertical redistribution of dust and the thermodynamic structure of the West Saharan atmospheric boundary layer during summer. IN Atmospheric Science Letters, 10. 34–42.
Added by: Boichard Jean-Luc 2010-08-05 10:13:46    Last Edited by: Fanny Lefebvre 2010-09-23 11:59:04
Categories: General
Keywords: AMMA
Creators: Cuesta, Flamant, Marsham, Parker
Collection: Atmospheric Science Letters

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The Saharan atmospheric boundary layer (SABL) plays a significant role in the atmospheric global circulation and directly affects the vertical redistribution of dust originated in the Sahara, the world's largest dust source. Recent measurements have revealed a variety of new dynamical mechanisms that control the structure of the SABL, which are responsible for exchange between the Saharan convective and residual boundary layers. Using new space-borne laser remote sensing data (CALIPSO) and recently published results, we provide an overview of the following known dynamical mechanisms: diurnal vertical mixing, dynamical lifting (density currents and cold air outbreaks) and topographic effects (mountains and albedo anomalies).
Added by: Fanny Lefebvre