Saharan dust transport and deposition towards the tropicalnorthern 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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fttibhannoverren:oai:oa.tib.eu:123456789/5449 2023-07-30T04:05:25+02:00 Saharan dust transport and deposition towards the tropicalnorthern Atlantic Schepanski, K. Tegen, I. MacKe, A. 2009 application/pdf https://oa.tib.eu/renate/handle/123456789/5449 https://doi.org/10.34657/4078 eng eng Göttingen : Copernicus ISSN:1680-7316 DOI:https://doi.org/10.5194/acp-9-1173-2009 https://doi.org/10.34657/4078 https://oa.tib.eu/renate/handle/123456789/5449 CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich Atmospheric Chemistry and Physics 9 (2009), 4 aerosol property atmospheric deposition atmospheric transport dust numerical model optical depth particulate flux suspended particulate matter vertical distribution Atlantic Ocean Atlantic Ocean (North) Cape Verde ddc:550 status-type:publishedVersion doc-type:article doc-type:Text 2009 fttibhannoverren https://doi.org/10.34657/407810.5194/acp-9-1173-2009 2023-07-10T16:19:23Z 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 Bod́eĺe Depression to Saharan dust over the Atlantic is investigated. A maximum contribution of Bod́eĺe dust transported towards the Cape Verde Islands is evident in winter when the Bod́eĺe 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. Article in Journal/Newspaper North Atlantic North Cape Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) North Cape ENVELOPE(165.700,165.700,-70.650,-70.650) |
institution |
Open Polar |
collection |
Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) |
op_collection_id |
fttibhannoverren |
language |
English |
topic |
aerosol property atmospheric deposition atmospheric transport dust numerical model optical depth particulate flux suspended particulate matter vertical distribution Atlantic Ocean Atlantic Ocean (North) Cape Verde ddc:550 |
spellingShingle |
aerosol property atmospheric deposition atmospheric transport dust numerical model optical depth particulate flux suspended particulate matter vertical distribution Atlantic Ocean Atlantic Ocean (North) Cape Verde ddc:550 Schepanski, K. Tegen, I. MacKe, A. Saharan dust transport and deposition towards the tropicalnorthern Atlantic |
topic_facet |
aerosol property atmospheric deposition atmospheric transport dust numerical model optical depth particulate flux suspended particulate matter vertical distribution Atlantic Ocean Atlantic Ocean (North) Cape Verde ddc: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 Bod́eĺe Depression to Saharan dust over the Atlantic is investigated. A maximum contribution of Bod́eĺe dust transported towards the Cape Verde Islands is evident in winter when the Bod́eĺe 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. |
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 tropicalnorthern Atlantic |
title_short |
Saharan dust transport and deposition towards the tropicalnorthern Atlantic |
title_full |
Saharan dust transport and deposition towards the tropicalnorthern Atlantic |
title_fullStr |
Saharan dust transport and deposition towards the tropicalnorthern Atlantic |
title_full_unstemmed |
Saharan dust transport and deposition towards the tropicalnorthern Atlantic |
title_sort |
saharan dust transport and deposition towards the tropicalnorthern atlantic |
publisher |
Göttingen : Copernicus |
publishDate |
2009 |
url |
https://oa.tib.eu/renate/handle/123456789/5449 https://doi.org/10.34657/4078 |
long_lat |
ENVELOPE(165.700,165.700,-70.650,-70.650) |
geographic |
North Cape |
geographic_facet |
North Cape |
genre |
North Atlantic North Cape |
genre_facet |
North Atlantic North Cape |
op_source |
Atmospheric Chemistry and Physics 9 (2009), 4 |
op_relation |
ISSN:1680-7316 DOI:https://doi.org/10.5194/acp-9-1173-2009 https://doi.org/10.34657/4078 https://oa.tib.eu/renate/handle/123456789/5449 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich |
op_doi |
https://doi.org/10.34657/407810.5194/acp-9-1173-2009 |
_version_ |
1772817306414481408 |