Response of Glacier and Lake Dynamics in Four Inland Basins to Climate Change at the Transition Zone between the Karakorum And Himalayas.

From 1968 to 2013, the AP of Shiquanhe station showed a decreasing trend at a rate of -0.423 mm a -1 (R 2 = 0.0352), whereas the AP of Hetian station and Yutian station showed increasing trends at rates of 0.476 mm a -1 (R 2 = 0.0594) and 0.547 mm a -1 (R 2 = 0.0453), respectively ( Fig 2D, 2E and 2F ).

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From 1968 to 2013, the MAT of Shiquanhe station, Hetian station and Yutian station all showed an increasing trend; the rates were 0.052°C a -1 (R 2 = 0.5522), 0.048°C a -1 (R 2 = 0.5809) and 0.054°C a -1 (R 2 = 0.1831), respectively ( Fig 2A, 2B and 2C ).

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