Calculation of wind speed in the 300-meter lower layer of the atmosphere based on the meteorological observations taking account of temperature stratification and surface roughness

Introduction. Taking into account relationship of wind profile power-law exponent (m) from hydrostatic stability of the layer and surface roughness the calculation method of wind speed and direction in the lower 300-meter layer of the atmosphere based on the meteorological observations is proposed....

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Bibliographic Details
Main Authors: S.N. Stepanenko, V.G. Voloshin, V. Yu. Kuryshina
Format: Article
Language:English
Published: Odessa State Environmental University 2016-07-01
Series:Український гідрометеорологічний журнал
Subjects:
Online Access:http://uhmj.org.ua/index.php/journal/article/view/35

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