G. Sauermann and H. J. Herrmann
Diploma Thesis
We work on models to describe the dynamics of the surface of
a dry granular bed, like a desert. These models, based on
coupled differential equations, can describe the formation
and evolution of dunes. The simplest and the most
well-known type of dunes is the Barchan dune which has the
shape of a crescent and occurs if the wind always comes from
the same direction and if there is not enough sand to cover
the entire surface. They are encountered typically close to the
ocean, for instance in Peru, Namibia and Morocco. On these fields
hundreds of Barchans can be found, generally all of the same size.
These dunes exist in heights between 1.5 m and 10 m, while their
basis is typically 40 to 150 m long and 30 to 100 m broad.
Field measurements have been performed in south Morocco
near Laâyoune to compare with the numerical
results. Figure
shows one of
these measured dunes.