Dry Deposition from Sahara Sources Regions of Western Africa

Sahara dust storms during March 2004 have attracted much attention from the dust-research community due to their intensity, wide coverage, and endurance. In the present work, the dry deposition mechanisms of mineral dust are analysed during an event on the 3 March 2004 over the Northwest African coa...

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Main Authors: B. Douaiba, A. Azzi, A. Khorsi, A. Benlefki
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2014/419838
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author B. Douaiba
A. Azzi
A. Khorsi
A. Benlefki
author_facet B. Douaiba
A. Azzi
A. Khorsi
A. Benlefki
author_sort B. Douaiba
collection DOAJ
description Sahara dust storms during March 2004 have attracted much attention from the dust-research community due to their intensity, wide coverage, and endurance. In the present work, the dry deposition mechanisms of mineral dust are analysed during an event on the 3 March 2004 over the Northwest African coast. This particular case was chosen based on the strong dry removal that occurred, rendering it ideal for examining the deposition processes. The simulation of synoptic conditions and dry deposition of four dust particles including clay, small silt, large silt, and sand was performed with Eta model, coupled with a desert dust cycle module. The results have been compared with surface data from weather stations in North Africa, data of dry metals from stations located in Gran Canaria, and various satellite images such as European Organization for the Exploitation of Meteorological Satellites and Moderate Resolution Imaging Spectroradiometer for the period in question.
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institution Kabale University
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publishDate 2014-01-01
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series Advances in Meteorology
spelling doaj-art-176cf95f5020461f9b325833bf9b566b2025-02-03T01:03:19ZengWileyAdvances in Meteorology1687-93091687-93172014-01-01201410.1155/2014/419838419838Dry Deposition from Sahara Sources Regions of Western AfricaB. Douaiba0A. Azzi1A. Khorsi2A. Benlefki3Faculty of Mechanical Engineering, University of Sciences and Technology of Oran, Oran, AlgeriaFaculty of Mechanical Engineering, University of Sciences and Technology of Oran, Oran, AlgeriaSchool in Science and Technology of Oran, AlgeriaAlgerian Petroleum Institute IAP, Arzew, Oran, AlgeriaSahara dust storms during March 2004 have attracted much attention from the dust-research community due to their intensity, wide coverage, and endurance. In the present work, the dry deposition mechanisms of mineral dust are analysed during an event on the 3 March 2004 over the Northwest African coast. This particular case was chosen based on the strong dry removal that occurred, rendering it ideal for examining the deposition processes. The simulation of synoptic conditions and dry deposition of four dust particles including clay, small silt, large silt, and sand was performed with Eta model, coupled with a desert dust cycle module. The results have been compared with surface data from weather stations in North Africa, data of dry metals from stations located in Gran Canaria, and various satellite images such as European Organization for the Exploitation of Meteorological Satellites and Moderate Resolution Imaging Spectroradiometer for the period in question.http://dx.doi.org/10.1155/2014/419838
spellingShingle B. Douaiba
A. Azzi
A. Khorsi
A. Benlefki
Dry Deposition from Sahara Sources Regions of Western Africa
Advances in Meteorology
title Dry Deposition from Sahara Sources Regions of Western Africa
title_full Dry Deposition from Sahara Sources Regions of Western Africa
title_fullStr Dry Deposition from Sahara Sources Regions of Western Africa
title_full_unstemmed Dry Deposition from Sahara Sources Regions of Western Africa
title_short Dry Deposition from Sahara Sources Regions of Western Africa
title_sort dry deposition from sahara sources regions of western africa
url http://dx.doi.org/10.1155/2014/419838
work_keys_str_mv AT bdouaiba drydepositionfromsaharasourcesregionsofwesternafrica
AT aazzi drydepositionfromsaharasourcesregionsofwesternafrica
AT akhorsi drydepositionfromsaharasourcesregionsofwesternafrica
AT abenlefki drydepositionfromsaharasourcesregionsofwesternafrica