The Saltating Particle Aleurite Mode in Wind–Sand Flux over a Desertified Area


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The saltating particle aleurite mode has been discovered in the wind–sand flux over a desertified area. The approximation of the measured saltating particle distribution was found using two lognormal distribution functions. In the wind–sand flux, the countable concentrations of aleurite and sand particles depend differently on the wind velocity in the atmospheric surface layer.

作者简介

G. Gorchakov

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017

D. Buntov

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017

A. Karpov

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017

V. Kopeikin

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017

S. Mirsaitov

MIREA Russian Technological University

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119454

R. Gushchin

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences; MIREA Russian Technological University

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017; Moscow, 119454

O. Datsenko

Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences; MIREA Russian Technological University

Email: gengor@ifaran.ru
俄罗斯联邦, Moscow, 119017; Moscow, 119454


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