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- W2350489128 abstract "With the contrastive analyses of the ice formation time,ice formation zones and the stratigraphic snow profiles,the constitution of the profiles,the distribution and the shift of dust layers and the ice layers within snow layers of the Glacier No.1 at the headwaters of the rumqi River,Tianshan Mountains,in different time(the 1960s and the 1980s and the beginning of this century),it is found that: since the 1960s,the snow depth on the glacier has decreased,the number and the buried depth of the dust layers and ice layers have decreased,and the profile constitution has changed with the increase of mean density.Ice formation zones have changed also.All the upper limitations of the zones are rising,and the cold percolation zone disappeared and was replaced by percolation zone.The most interesting thing is that the top of the east branch was replaced by an ablation area.With a new method——tracking the marks buried in snow profiles,the ice formation time was determined to be 3.5～4 years.The change of heat state in the snow profiles caused by climate change,especially the temperature rising,is the main reason for the changes.Temperature rising results in more snow melted,and causes the decrease of snow depth,decrease or disappearance of dust layers and ice layers." @default.
- W2350489128 created "2016-06-24" @default.
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- W2350489128 date "2007-01-01" @default.
- W2350489128 modified "2023-09-23" @default.
- W2350489128 title "A Contrast of the Ice Formation Time,Ice Formation Zones and the Stratigraphic Profiles of Snow Pits in Different Time of the Glacier No.1 at the Headwaters of the rümqi River,Tianshan Mountains" @default.
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