Discussing Sources of Moisture Feeding the Glaciers on the Eastern Qangtang Plateau
Discussing Sources of Moisture Feeding the Glaciers on the Eastern Qangtang Plateau
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发表时间：
2012
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通讯作者：
Dong Guo-cheng
中科院分区：
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作者：
Dong Guo-cheng
本文应用地貌学方法研究了青藏高原腹地的四座高山。四座高山中，山脊自南向北的高山东坡冰川发育，山脊自西向东的高山南坡冰川发育，且南北向冰川面积较大。沿着纬度方向，雪线高度在88° E以西基本不变，而在88° E以东由西向东急剧降低。青藏高原东部冰川的水分来源于东南方向，印度季风
In this paper,four mountains in the interior of the Tibetan Plateau were researched with geomorphological methods.Among the four mountains,those with ridges from south to north have glaciers well developed on the east slopes,and those with ridges from west to east have glaciers well developed on the south slopes.Furthermore,glaciers with south and east aspects occupy much more area.Along the latitudinal direction,altitude of snowline is almost the same in the west of 88° E,but decreases sharply from west to east in the east of 88° E.Along the longitudinal direction,altitude of snowline first increases and then decreases from south to north.All the information indicates that moisture feeding the glaciers in the east of Qangtang Plateau comes from the southeast by the Indian monsoon.