Junchao Shi

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Accumulation gain is essential for mass balance of valley glaciers in the Karakoram Himalayas. The higher elevation of this area received snowfall(>1000 cm · yr−1) annually, while the snowfall occupies 95% of total precipitation (75-150 cm · yr−1). Meanwhile, the air temperature ranging from -20 to -40 °C, during DecemberFebruary, is also very suitable for(More)
Glaciers in the Tibetan mountains are expected to be sensitive to climate change. The change of glacier mass is locally depending on e.g. precipitation, melting and variation in ice flow. In this paper we analyze the data acquired by ICESat/GLAS laser altimetry, along several tracks over the glaciers of the Nyainqêntanglha range from February, 2003(More)
The polythermal glacier is one of the dominant glaciers distributed widely in the transition zone of monsoon and continental climate, Tibetan Plateau. However, the glacier dynamics study of this type glacier is still limited in most of glaciated area due to the remote mountains, and high altitude issues. Meanwhile, the surface displacement of polythermal(More)
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