Editorial Type:
Article
Article Type:
Research Article

The Diurnal and Seasonal Cycles of Wind-Borne Dust over Africa North of the Equator

G. N’Tchayi Mbourou Faculté des Sciences, Universite des Sciences et Techniques de Masuku, Franceville, Gabon

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J. J. Bertrand Faculté des Sciences, Universite de Niamey, Niamey, Niger

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S. E. Nicholson Department of Meteorology, The Florida State University, Tallahassee, Florida

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Print Publication:
01 Jul 1997
DOI:
https://doi.org/10.1175/1520-0450(1997)036<0868:TDASCO>2.0.CO;2
Page(s):
868–882
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Abstract

This article presents a study of the diurnal and seasonal cycles of dust over North Africa, using surface visibility as an indicator of dust. The diurnal cycle shows a reduction of visibility during the daytime hours in the areas where dust is generated, a consequence of the elimination of the nocturnal inversion. The annual cycle reveals that, at latitudes from 5° to 16°N, there is a latitudinal increase in the duration of the presence of aerosols over the course of the year. The presence of aerosols dimishes in the latitudes from 20° to 35°N, indicating that the aerosol content of the Saharan air is lower than that over the semiarid sub-Saharan zones, such as the Sahel. A comparison of three periods, 1957–61, 1970–74, and 1983–87, shows a continually increasing presence of dust, particularly in the western Sahel. The interannual variability of the dust and its annual cycles in these three periods throughout North Africa bear a strong relationship to rainfall fluctuations in the Sahel. Overall, the results indicate that over the last few decades the Sahel region has replaced the central Sahara as the source of atmospheric aerosols over most of North Africa.

Corresponding author address: Dr. Sharon E. Nicholson, Dept. of Meteorology, B-161, The Florida State University, Tallahassee, FL 32306-3034.

Abstract

This article presents a study of the diurnal and seasonal cycles of dust over North Africa, using surface visibility as an indicator of dust. The diurnal cycle shows a reduction of visibility during the daytime hours in the areas where dust is generated, a consequence of the elimination of the nocturnal inversion. The annual cycle reveals that, at latitudes from 5° to 16°N, there is a latitudinal increase in the duration of the presence of aerosols over the course of the year. The presence of aerosols dimishes in the latitudes from 20° to 35°N, indicating that the aerosol content of the Saharan air is lower than that over the semiarid sub-Saharan zones, such as the Sahel. A comparison of three periods, 1957–61, 1970–74, and 1983–87, shows a continually increasing presence of dust, particularly in the western Sahel. The interannual variability of the dust and its annual cycles in these three periods throughout North Africa bear a strong relationship to rainfall fluctuations in the Sahel. Overall, the results indicate that over the last few decades the Sahel region has replaced the central Sahara as the source of atmospheric aerosols over most of North Africa.

Corresponding author address: Dr. Sharon E. Nicholson, Dept. of Meteorology, B-161, The Florida State University, Tallahassee, FL 32306-3034.

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Journal of Applied Meteorology and Climatology

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