The Saltating Particle Aleurite Mode in Wind–Sand Flux over a Desertified Area
- Авторы: Gorchakov G.I.1, Buntov D.V.1, Karpov A.V.1, Kopeikin V.M.1, Mirsaitov S.F.2, Gushchin R.A.1,2, Datsenko O.I.1,2
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Учреждения:
- Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
- MIREA Russian Technological University
- Выпуск: Том 488, № 1 (2019)
- Страницы: 1103-1106
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/195454
- DOI: https://doi.org/10.1134/S1028334X19090149
- ID: 195454
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Аннотация
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.
Об авторах
G. Gorchakov
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: gengor@ifaran.ru
Россия, Moscow, 119017
D. Buntov
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Email: gengor@ifaran.ru
Россия, Moscow, 119017
A. Karpov
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Email: gengor@ifaran.ru
Россия, Moscow, 119017
V. Kopeikin
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Email: gengor@ifaran.ru
Россия, Moscow, 119017
S. Mirsaitov
MIREA Russian Technological University
Email: gengor@ifaran.ru
Россия, Moscow,
119454
R. Gushchin
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences; MIREA Russian Technological University
Email: gengor@ifaran.ru
Россия, Moscow, 119017; Moscow,
119454
O. Datsenko
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences; MIREA Russian Technological University
Email: gengor@ifaran.ru
Россия, Moscow, 119017; Moscow,
119454
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