A name for silt and clay deposited by wind. It forms
a uniform blanket that covers hills and valleys at many altitudes,
which distinguishes it from deposits of streams. Strong
winds that blow across desert regions sometimes pick up dust
made of silt and clay particles and transport them thousands
of kilometers from their source. For instance, dust from
China is found in Hawaii, and the Sahara commonly drops
dust in Europe. This dust is a nuisance, has a significant
influence on global climate, and has, at times, as in the dust
bowl days of the 1930s, been known to nearly block out the
sun.
Recently, it has been recognized that windblown dust
contributes significantly to global climate. Dust storms that
come out of the Sahara can be carried around the world and
can partially block out some of the Sun’s radiation. The dust
particles may also act as small nuclei for raindrops to form
around, perhaps acting as a natural cloud-seeding phenomenon.
One interesting point to ponder is that as global
warming increases global temperatures, the amount and
intensity of storms increase, and some of the world’s deserts
expand. Dust storms may serve to reduce global temperatures
and increase precipitation. In this way, dust storms may represent
some kind of self-regulating mechanism, whereby the
Earth moderates its own climate.
See also DESERT.
longshore drift See LITTORAL.














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