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- W2392684098 abstract "Under global warming and climatic shift to warm-wet in the west regions of Northwest China in the 1980s, it is interested to know the recent variation of glacier in the Tarim River drainage. For analyzing the variation characteristics of climate and the factors affecting ablation, the mass balance, ice movement, hydrology, meteorology and so on were studied on a typical glacier the Keqicar Glacier. It is very important to research the mechanics of the glacier responding to climate change and the impact upon the water resources of the Tarim River. On the Keqicar Glacier there is much high air temperature in summer, higher than 0 ℃ all day long basically, and low diurnal range, so the daily ablation on the glacier terminal is very large as compared with adjacent glaciers. The lapse rate of are temperature is low, about 0.60 ℃·(100m)~(-1), so cold effect of glacier is not obvious. Local circulation——mountain-valley wind develops on the glacier; Influence of westerly is evident above 4 250 m a. s. l. The convectional precipitation is much more, 75% of which occurs in daytime, because there is much more cumulonimbus and convectional airflow. Diurnal variation of relative humidity is obvious and increases with altitude. Net radiation is lager in July and the first/middle ten days of August, and then radiation begins to decrease from the last ten days of August, which coincides with the ablation of glacier. Ablation is very strong from July 1~(st) to July 26~(th), with a mean ablation rate of 38.66 mm·d~(-1), then the rate decreases a little to the middle ten days of August, about 34.79 mm·d~(-1), and finally the rate decreases rapidly to the middle ten days of September, about 28.83 mm·d~(-1)." @default.
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- W2392684098 date "2004-01-01" @default.
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- W2392684098 title "Characteristics of Climate on the Keqicar Glacier on the South Slopes of the Tianshan Mountains during Ablation Period" @default.
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