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《Journal of Glaciology and Geocryology》 2005-04
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Interdecadal Variability of Seasonal Frozen Ground Depth and Its Climatic Reasons in Hexi Corridor of Gansu

GUO Hui~\{1, 2\},LI Dong-liang~1,ZHANG Qiang~2,LU Deng-rong~3,FEN Jian-ying~1,QING Ji-zu~2,TANG Mao-chang~1,SHEN Zhi-bao~1(1. Key Laboratory of Arid Climatic Changing and Reducing Disaster of Gansu Province, Cold and Arid Regions Environmental andEngineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000,China; 2. Key Laboratory of AridClimatic Changing and Reducing Disaster of Gansu Province, Arid Meteorological Research Institute of ChinaMeteorological Adminstration, Lanzhou Gansu 730020, China; 3. Central Information and Networkof Gansu Province Meteorological Bureau, Lanzhou Gansu 730020, China)  
Analyzing the upper and lower limits of seasonal frozen ground depth, its main frozen period and ending date from 1958 to 2003 of 17 representative meteorological stations in Hexi Corridor of Gansu Province demonstrates that the change of seasonal maximum frozen ground depth has an 810 a period; There was a shift of the frozen ground depth in the mid 1980s, showing a winter temperature warming in Hexi Corridor of Gansu Province since the mid 1980s. The minimum air temperature in winter controls the seasonal frozen ground depth and its main frozen period. The thaw of frozen ground depends on the ground temperature in winter, with a pronounced negative correlation. Especially, the difference among the 5 cm ground temperature and the 1.5 m air temperature above surface, as well as the daily range of temperature in winter is more correlative to the frozen ground depth in Heixi Corridor of Gansu Province.
【Fund】: 国家科技部攻关“西部开发科技行动”重大项目(2004BA901A16);; 甘肃自然科技开发基金项目(3ZS041-A25-013)资助
【CateGory Index】: P343.1
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