Predominant transport paths of Saharan dust over the Mediterranean Sea to Europe

We use monthly data of aerosol optical thickness (AOT) from the Moderate Resolution Imaging Spectroradiometer on board the seven NASA Terra and Aqua satellites for a 10 year period (2001–2010) in order to determine seasonal variations of Saharan dust transport over the Mediterranean toward Europe. T...

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Veröffentlicht in:Journal of Geophysical Research: Atmospheres 2012-01, Vol.117 (D2), p.n/a
Hauptverfasser: Israelevich, P., Ganor, E., Alpert, P., Kishcha, P., Stupp, A.
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Sprache:eng
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Zusammenfassung:We use monthly data of aerosol optical thickness (AOT) from the Moderate Resolution Imaging Spectroradiometer on board the seven NASA Terra and Aqua satellites for a 10 year period (2001–2010) in order to determine seasonal variations of Saharan dust transport over the Mediterranean toward Europe. The maxima of AOT are used to visualize the transport paths. Saharan dust reaches Europe over the Mediterranean and also by looping back over the Atlantic. In spring, aerosols are observed within a wide range of longitudes in Europe, with the highest AOT over western Europe. This may be partially explained by dust transport to western Europe via the Atlantic route, while to central and eastern Europe, dust is transported over the Mediterranean. During all seasons, dust is transported over the Mediterranean to Europe. In the summer months, aerosols are observed predominantly in central Europe. In autumn, aerosol activity is strongest in eastern Europe. We show that there are local AOT maxima over north Italy, in the Alps, in Spain, southeast of the Pyrenees and Sierra Nevada, and in the Rila Mountains in Bulgaria. We suggest that these maxima of aerosol concentration appear as the dust‐carrying airflow reaches the mountains and slows. Key Points Major transport routes of dust over Mediterranean for different seasons Amount of dust transported during dust events is minor part of annual transport Desert dust may accumulate in front of mountain chains
ISSN:0148-0227
2169-897X
2156-2202
2169-8996
DOI:10.1029/2011JD016482