Though we didn't realize it, the haze that has been over Cape Verde these last few days has been caused by this. It also explains why all the smoke alarms in the missionary's apartments are going off. Ugh.
ACCUWEATHER - The
Saharan Air Layer, or known more commonly as Saharan Dust, is a layer of tiny
aerosols like sand, dirt and dust that occasionally push from east to west
across the tropical Atlantic Ocean during hurricane season. These aerosols
originate over the very hot and dry deserts of Africa, like the Saharan Desert,
and sometimes get picked up by African easterly waves which push westward from
Africa into the Atlantic Ocean.
The Saharan Air Layer is
a well-mixed dry pocket of air that usually resides between 5,000 and 15,000
feet above sea level. Since one of the key ingredients for tropical cyclone
development is a deep feed of moisture, Saharan Dust often acts to inhibit tropical
development. Research suggests that there are three main reasons Saharan Dust
has a negative impact on tropical development:
1) A surge in the
mid-level African easterly jet increases the vertical wind shear.
2) The inclusion, or
drawing in, of dry air into a tropical system.
3) An enhanced trade
wind inversion which acts to stabilizes the atmosphere. A stable atmosphere
will make it more difficult for deep convection to develop.
Once a pocket of Saharan
Dust begins moving westward over the Atlantic Ocean, it is relatively easy to
track by using certain infrared satellite products. The algorithm in some
infrared products is sensitive to dry, dusty air and, therefore, can track when
pockets of this kind of air move from place to place.
Many factors go into
forecasting the track and strength of a tropical system. Knowing whether or not
a tropical cyclone will have Saharan Dust in its vicinity is one factor that
can determine the cyclone's intensity.
Online:
http://www.accuweather.com/en/weather-news/watch-massaive-saharan-dust-cl/16065339
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