by Jochen Kerkmann (EUMETSAT) and Martin Setvak (CHMI)
Jump to imagesAs shown in the image of the month Wind-driven land surface features in the Sahara desert, the Borkou region in Northern Chad between the Tibesti Mountains (3415 m) and Ennedi Mountains (1450 m) represents a "bottleneck" for the low-level winds that approach this region from the northeast. As this orographic low-level jet blows further south, exiting the Borkou "bottleneck", by coincidence it passes above the Bodele Depression - a dried salty lake, which serves as a very efficient source of small particles for local dust storms. According to NASA experts, "the dry bowl that forms the Bodele Depression is one of the most active sources of wind-blown dust in the world. The depression is marked by a series of ephemeral lakes, which may be infrequently flooded with mud-laden water from the mountains. When the lakes dry, a layer of loose clay is left behind. The dirt is easily carried on the wind that blows down from the mountains".
The Meteosat-8 images below show a major (continental-scale) dust outbreak that occurred in the beginning of January 2005. As discussed above, huge quantities of dust get picked up in the Bodele Depression and carried towards Niger and Nigeria. Another area where dust easily gets picked up is the area of Agadez (Niger), to the northwest of the Bodele Depression. As the fine dust particles serve as a passive tracer, they nicely show the channelled airflow (streamlines) in the Borkou area and around the major mountain ranges (Tibesti, Massif de l'Air) in the Central Sahara.
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