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- W2368962786 abstract "How to fix on the confine of freezing-thaw erosion zone in Qinghai-Tibet Plateau is one of the questions need to be resolved chiefly.Based on the author's and former researchers'work,the theory foundation of freezing-thaw erosion zoning in Qinghai-Tibet Plateau was proposed.Then the area of freezing-thaw erosion in Tibet was defined by using GIS software.By analyzing the distribution of freezing-thaw erosion area,this paper pointed out any characters of freezing-thaw erosion area in Tibet as follows:1) The area of freezing-thaw erosion is very large,accounts 55 3 percent of area of Tibet.2) The difference between north and south Brahmaputra River is obvious.The freezing-thaw area is large and distributing continuously in north Brahmaputra River,but small and distributing like island in south Brahmaputra River.3) The difference among regions is also obvious.The freezing-thaw erosion area is most concentrated in Nakchu and Ngari.4) Freezing-thaw erosion is the main erosion type in Nakchu,Ngari,Lhasa,Chamdo and Shigatse,but is not in Lhoka and Nyingtri." @default.
- W2368962786 created "2016-06-24" @default.
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- W2368962786 date "2005-01-01" @default.
- W2368962786 modified "2023-09-24" @default.
- W2368962786 title "A New Way for Definiting the Freezing-Thaw Erosion Area in Tibet" @default.
- W2368962786 hasPublicationYear "2005" @default.
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