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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ftleibnizopen:oai:oai.leibnizopen.de:EEGWhIgBdbrxVwz6VC73 2023-06-18T03:41:59+02:00 Saharan dust transport and deposition towards the tropical northern Atlantic Schepanski, K. Tegen, I. Macke, A. 2009 application/pdf https://doi.org/10.34657/1242 https://oa.tib.eu/renate/handle/123456789/407 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Atmospheric Chemistry and Physics, Volume 9, Issue 4, Page 1173-1189 550 article Text 2009 ftleibnizopen https://doi.org/10.34657/1242 2023-06-04T23:27:33Z 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. publishedVersion Article in Journal/Newspaper North Atlantic LeibnizOpen (The Leibniz Association) |
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English |
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550 Schepanski, K. Tegen, I. Macke, A. Saharan dust transport and deposition towards the tropical northern Atlantic |
topic_facet |
550 |
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. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Schepanski, K. Tegen, I. Macke, A. |
author_facet |
Schepanski, K. Tegen, I. Macke, A. |
author_sort |
Schepanski, K. |
title |
Saharan dust transport and deposition towards the tropical northern Atlantic |
title_short |
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_sort |
saharan dust transport and deposition towards the tropical northern atlantic |
publisher |
München : European Geopyhsical Union |
publishDate |
2009 |
url |
https://doi.org/10.34657/1242 https://oa.tib.eu/renate/handle/123456789/407 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Atmospheric Chemistry and Physics, Volume 9, Issue 4, Page 1173-1189 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.34657/1242 |
_version_ |
1769007747915841536 |