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Study on the Spa tia l Var ia tion of Annua l Prec ip ita tion Structure over Gan su Prov ince Dur ing Recen t 46 Years
HAN  Hui, MENG Li-Xia
Journal of Arid Meteorology    2010, 28 (1): 30-34.  
Abstract1825)      PDF(pc) (641KB)(2427)       Save

Based on the analysis of daily p recip itation of 62 weather stations in Gansu Province from 1960 to 2005, it educed the characteristics of spatial variation of different intensity p recip itation days and p recip itation relative extremes, and those can reflect the structure of p recip itaiton. The results show that there isn’t any homogeneous variation over the whole p rovince for each indicator, and the spatial distinction of p recip itation variation is great. Thus, the regional average of p recip itation ismeaningless and the structure ismore powerful to exp lain the change of p recip itation, for which decomposed the dim unitary situation into vivid particular phenomena. The farther research on spatial variation of p recip itation structure indicates that a significant variation of p recip itation in a specific region is a synthetical consequence of the interactions among all indicators. This synthesis p rocedure is very comp licated, and usually has not broad rep resentation. Even nonsignificant variation of each indicator can bring forth a significant variation of p recip itation.

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Compara tive Ana lysis on W ind Da ta from Atmospheric Wind Prof iler and Ba lloon Sound ing
SUN Xu-Yang, HAN  Hui, DUAN Hai-Xia, ZHANG  Liang, LI Yi-Beng, YAN Jing-Ze, JU Yong-Xin
J4    2008, 26 (3): 48-52.  
Abstract1839)      PDF(pc) (598KB)(2523)       Save

Firstly,the working p rincip le and measurement p recision of the Airda - 3000Q type atmospheric wind p rofiler (AWP) were introduced. Then, a contradistinctive analysis on the wind p rofile data acquired by both AWP and synchronous balloon sounding was conducted to estimate the reliability ofAWP for detectingwind field. The results show that under the stable weather condition, the p rofiler’s detection ofwind direction and wind speed had some deviation compared by the balloon’s detection from the ground to 200 m height due to the detecting blind spots of the AWP and the ground clutter, but above 200 m, both wind field p rofiles correlated well;Under the comp lex weather condition, theirwind p rofiles had obvious deviation because the wind information on the different height acquired by AWP is a temporal average of wind field in a time period, but the wind data measured by sounding balloon on a specific height is the instantaneous value while balloon passed by.

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