Saltating particle aleurite mode in windsand flux over desertified area

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Abstract

Saltating particle aleurite mode is discovered in the windsand flux over desertified area. Approximation of the saltating particle distribution measured is received using two lognormal distribution functions. It is shown that aleurite and sand number concentration particles in the windsand flux depends on wind velocity in the surface layer in different way.

About the authors

G. I. Gorchakov

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences

Author for correspondence.
Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017

D. V. Buntov

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences

Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017

A. V. Karpov

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences

Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017

V. M. Kopeikin

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences

Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017

S. F. Mirsaitov

"MIREA-Russian Technological University"

Email: gengor@ifaran.ru
Russian Federation, 78, Vernadskogo prospect, Moscow, 119454

R. A. Gushchin

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences; “MIREA-Russian Technological University”

Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017; 78, Vernadskogo prospect, Moscow, 119454

O. I. Datsenko

Obukhov Institute of Atmospheric Physics of the Russian Academy of Sciences; “MIREA-Russian Technological University”

Email: gengor@ifaran.ru
Russian Federation, 3, Pizevsky, Moscow, 119017; 78, Vernadskogo prospect, Moscow, 119454

References

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