Anomaly feature of seasonal frozen soil variations on the Qinghai-Tibet Plateau

[1]Betts A K, H Ball A C, M Beljaars et al., 1996. The land surface-atmosphere interaction: a review based on observational and global modeling. Journal of Geophysical Research, 101: 7209-7225. [2]Cheng Guodong, 1990. Recent development of geocryological study in China. Acta Geographica Sinica, 45 (...

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Published in:Journal of geographical sciences 2002, Vol.12 (1), p.99-107
Main Author: WANG Cheng-hai
Format: Article
Language:eng
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Summary:[1]Betts A K, H Ball A C, M Beljaars et al., 1996. The land surface-atmosphere interaction: a review based on observational and global modeling. Journal of Geophysical Research, 101: 7209-7225. [2]Cheng Guodong, 1990. Recent development of geocryological study in China. Acta Geographica Sinica, 45 (2): 220-224. (in Chinese) [3]Dai Jiaxi, 1990. Climatology of Tibetan Plateau. Beijing: Meteorological Press. (in Chinese) [4]Goodrich K E, 1982. The influence of snow cover on the ground thermal region. Canadian Geotechnical Journal, 19: 421-432. [5]Horel D, 1981. A rotated principal component analysis of the interannual variability of Northern Hemisphere 500 hPa high field. M.W.R., 109: 2080-2091. [6]Jin Huijun, Li Shuxun, Wang Shaoling et al., 2000. Impacts of climate change on permafrost and cold regions environments in China. Acta Geographica Sinica, 55 (2): 161-173. (in Chinese) [7]Keith A Cherkauer, Dennis P Lettenmaier, 1999. Hydrologic effects of frozen soils in the upper Mississippi River basin. Journal of Geophysical Research, 104 (D16): 19,599-19,610. [8]Li Shude, Cheng Guodong, 1996. Map of Permafrost on Qinghai-Tibetan (1:3,000,000). Lanzhou: Gansu Culture Press. (in Chinese). [9]Li Shuxun, 1996. Approximately analysing the future thermal regime of permafrost on the Tibetan Plateau under climate warming. Proceeding of the Fifth National Conference on Glaciology and Geocryology (Vol.1). Lanzhou: Gansu Culture Press, 27-34. (in Chinese) [10]North G, T Bell, R Cahalan et al., 1982. Sampling errors in the estimation of empirical orthogonal function. M.W.R., 110: 699-760. [11]Pavlov A V, 1994. Current change of climate and permafrost in the Arctic and Sub-Arctic of Russia. Permafrost and Periglacial Processes, 5: 101-110. [12]Slater A G, Pitman A G, Desborough C E, 1998. Simulation of freeze-thaw cycles in a general circulation model land surface scheme. Journal of Geophysical Research, 103 (D10): 11303-11312. [13]Wang Chenghai, Dong Wenjie, Wei Zhifgang, 2001. The feature of seasonal frozen soil in Qinghai-Tibet Plateau. 56 (5): 523-531. (in Chinese) [14]Wang Shaoling, 1996. An approach on permafrost degradation and enviromental problems in the Tibetan plateau. Proceeding of the Fifth National Conference on Glaciology and Geocryology (Vol.1). Lanzhou: Gansu Culture Press, 11-17. (in Chinese) [15]Zhou Youwu, Gao Xingwang, Wang Yinxue, 1996. The ground temperature changes of seasonally freeze-thaw layers and climate warming in Northeast China in the past
ISSN:1009-637X
1861-9568