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Diurnal Variation of Atmospheric Water Vapor Content in 2009 over Taklimakan Desert
CUI Li-Na, SHI Yu-Guang, CUI Cai-Xia, DIAO Ling, LI Yan-Yong
J4    2010, 28 (4): 407-410.  
Abstract1110)      PDF(pc) (333KB)(1841)       Save

By using the GAMIT soft,the water vapor content of atmosphere was retrieved based on the ground-based GPS data from January to October 2009 in Tazhong station.The diurnal variation curve of PW were obtained by analyzing averaged data of each month.The results are as follows:the diurnal variation of the whole year’s water vapor content in the hinterland of the Taklimakan Desert was obvious and it presented a sine curve.The maximum appears at 08:00 and 23:00 with the values of 13.63 mm and 13.85 mm.The minimum appears at 01:00 and 14:00,12.91 and 12.28 mm,respectively.Atmospheric water vapor content is the least in January with the average value of 7.09 mm,and the minimum value was 0.95 mm at 13:00 on January 21 in winter of 2009.And it is the most in July with the value of 20.01 mm,the maximum value is 34.75 mm at 07:00 on August 6 in summer of 2009.The maximum diurnal variation range of water vapor content is in October,and there is not significant fluctuations in February.

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