Saharan dust transport and deposition towards the tropical northern Atlantic

We present a study of Saharan dust export towards the tropical North Atlantic using the regional dust emission, transport and deposition model LM-MUSCAT. Horizontal and vertical distribution of dust optical thickness, concentration, and dry and wet deposition rates are used to describe seasonality o...

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Main Authors: K. Schepanski, I. Tegen, A. Macke
Format: Article
Language:English
Published: Copernicus Publications 2009-02-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/9/1173/2009/acp-9-1173-2009.pdf
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author K. Schepanski
I. Tegen
A. Macke
author_facet K. Schepanski
I. Tegen
A. Macke
author_sort K. Schepanski
collection DOAJ
description We present a study of Saharan dust export towards the tropical North Atlantic using the regional dust emission, transport and deposition model LM-MUSCAT. Horizontal and vertical distribution of dust optical thickness, concentration, and dry and wet deposition rates are used to describe seasonality of dust export and deposition towards the eastern Atlantic for three typical months in different seasons. Deposition rates strongly depend on the vertical dust distribution, which differs with seasons. Furthermore the contribution of dust originating from the Bodélé Depression to Saharan dust over the Atlantic is investigated. A maximum contribution of Bodélé dust transported towards the Cape Verde Islands is evident in winter when the Bodélé source area is most active and dominant with regard to activation frequency and dust emission. Limitations of using satellite retrievals to estimate dust deposition are highlighted.
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spelling doaj.art-95f8a33121dc4e63b4f4c120d829d96c2022-12-21T19:40:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242009-02-019411731189Saharan dust transport and deposition towards the tropical northern AtlanticK. SchepanskiI. TegenA. MackeWe present a study of Saharan dust export towards the tropical North Atlantic using the regional dust emission, transport and deposition model LM-MUSCAT. Horizontal and vertical distribution of dust optical thickness, concentration, and dry and wet deposition rates are used to describe seasonality of dust export and deposition towards the eastern Atlantic for three typical months in different seasons. Deposition rates strongly depend on the vertical dust distribution, which differs with seasons. Furthermore the contribution of dust originating from the Bodélé Depression to Saharan dust over the Atlantic is investigated. A maximum contribution of Bodélé dust transported towards the Cape Verde Islands is evident in winter when the Bodélé source area is most active and dominant with regard to activation frequency and dust emission. Limitations of using satellite retrievals to estimate dust deposition are highlighted.http://www.atmos-chem-phys.net/9/1173/2009/acp-9-1173-2009.pdf
spellingShingle K. Schepanski
I. Tegen
A. Macke
Saharan dust transport and deposition towards the tropical northern Atlantic
Atmospheric Chemistry and Physics
title Saharan dust transport and deposition towards the tropical northern Atlantic
title_full Saharan dust transport and deposition towards the tropical northern Atlantic
title_fullStr Saharan dust transport and deposition towards the tropical northern Atlantic
title_full_unstemmed Saharan dust transport and deposition towards the tropical northern Atlantic
title_short Saharan dust transport and deposition towards the tropical northern Atlantic
title_sort saharan dust transport and deposition towards the tropical northern atlantic
url http://www.atmos-chem-phys.net/9/1173/2009/acp-9-1173-2009.pdf
work_keys_str_mv AT kschepanski saharandusttransportanddepositiontowardsthetropicalnorthernatlantic
AT itegen saharandusttransportanddepositiontowardsthetropicalnorthernatlantic
AT amacke saharandusttransportanddepositiontowardsthetropicalnorthernatlantic