Generation of wind waves by vortices in a retarding flow of air


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Abstract

It is shown that stable waves are generated on a water surface induced by a horizontal airflow whose speed falls along the flux under certain conditions: the period of chain of vortices generated in a viscous layer of airflow coincides with that of a group of waves with a length corresponding to the distance between the vortices. The dependence of a stable wave on the speed and drop in speed of a slowing airflow is obtained.

About the authors

O. N. Melnikova

Faculty of Physics, Department of the Physics of Sea and Inland Waters

Author for correspondence.
Email: olamel@yandex.ru
Russian Federation, Moscow, 119991

K. V. Pokazeev

Faculty of Physics, Department of the Physics of Sea and Inland Waters

Email: olamel@yandex.ru
Russian Federation, Moscow, 119991

M. N. Shabrov

Faculty of Physics, Department of the Physics of Sea and Inland Waters

Email: olamel@yandex.ru
Russian Federation, Moscow, 119991

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