Articles | Volume 17, issue 17
Atmos. Chem. Phys., 17, 10223–10243, 2017

Special issue: The Saharan Aerosol Long-range Transport and Aerosol-Cloud-interaction...

Atmos. Chem. Phys., 17, 10223–10243, 2017

Research article 01 Sep 2017

Research article | 01 Sep 2017

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

Kerstin Schepanski et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Kerstin Schepanski on behalf of the Authors (31 Jul 2017)  Author's response    Manuscript
ED: Publish as is (03 Aug 2017) by Cyrille Flamant
Short summary
This study illustrates the complexity of the interaction among the three major circulation regimes stimulating the North African dust outflow: harmattan, Saharan heat low, and monsoon circulation. We analyse fields from model simulations and satellite observations in concert in order to link atmospheric circulation and dust source activation as well as to characterize their impact on the variability of the dust outflow towards the Atlantic.
Final-revised paper