Water-vapor content in the atmosphere of arid zone

被引：0
|
作者：
S. F. Abdullaev
V. A. Maslov
B. I. Nazarov
T. Kh. Salikhov
机构：
[1] Tajik Academy of Sciences,Umarov Institute of Physics and Technology
[2] Scientific Research Institute of Tajik National University,undefined
来源：
Izvestiya, Atmospheric and Oceanic Physics | 2014年 / 50卷
关键词：
water vapor; moisture content; dust haze; aerosol; seasonal variation; air temperature;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
The variation in water-vapor content W in the atmosphere of the arid zone is studied. The seasonal oscillations in W for the arid zone are characterized by changes in the moisture content from 2.3 to 3.6 times during the transition from winter to summer. The summer-fall period is characterized by a well-expressed midday minimum of moisture content. In winter the moisture content monotonically decreases during the day. In spring the water-vapor content has a wide maximum in midday. The water-vapor content in the atmosphere during dust haze increases up to two times.
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页码：179 / 187
页数：8
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