Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
Abstract
In the present work the wind dynamics in the atmospheric boundary layer is studied; it is shown that wind slope angle at the ground surface with respect to isobars depends on the horizontal pressure gradients along parallel and meridian and not always equal to 45°.
About the Authors
Yuliya Aleksandrovna Semenova
Северо-Кавказский федеральный университет
Russian Federation
Russian Federation
Kristina Stanislavovna Avakyan
Северо-Кавказский федеральный университет
Russian Federation
Russian Federation
Robert Gurgenovich Zakinyan
Северо-Кавказский федеральный университет
Russian Federation
Russian Federation
References
1. Руководство по краткосрочным прогнозам погоды. Ленинград: Гидрометиздат, 1986. Ч. I. 704 с
2. Тверской П. Н. Курс метеорологии (физика атмосферы). Ленинград: Гидрометиздат, 1962. 700 с.
Review
For citations:
Semenova Yu.A., Avakyan K.S., Zakinyan R.G. Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations. Science. Innovations. Technologies. 2013;(1):26-29. (In Russ.)
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