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....
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Odessa State Environmental University
2016-07-01
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Series: | Український гідрометеорологічний журнал |
Subjects: | |
Online Access: | http://uhmj.org.ua/index.php/journal/article/view/35 |