Initial estimate of the contribution of cryospheric change in China to sea level rise
Jiawen Ren, Baisheng Ye, Yongjian Ding, Shiyin Liu
Abstract
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Jiawen Ren, Baisheng Ye, Yongjian Ding, Shiyin Liu
Abstract
Open-access reader
Recent studies have shown that cryospheric melting is becoming the dominant factor responsible for sea level rise, and that the melt-water from mountain glaciers and ice caps has comprised the majority of the cryospheric contribution since 2003. Analysis of the estimations of cryospheric melt-water and precipitation in glacier regions indicated that the potential contribution of the cryosphere in China is 0.14 to 0.16 mm a −1 , of which approximately 0.12 mm a −1 is from glaciers. The contribution of glaciers in the outflow river basins is about 0.07 mm a −1 , accounting for 6.4% of the total from global glaciers and ice caps.
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Recent studies have shown that cryospheric melting is becoming the dominant factor responsible for sea level rise, and that the melt-water from mountain glaciers and ice caps has comprised the majority of the cryospheric contribution since 2003. Analysis of the estimations of cryospheric melt-water and precipitation in glacier regions indicated that the potential contribution of the cryosphere in China is 0.14 to 0.16 mm a −1 , of which approximately 0.12 mm a −1 is from glaciers. The contribution of glaciers in the outflow river basins is about 0.07 mm a −1 , accounting for 6.4% of the total from global glaciers and ice caps.
Key concepts: Glacier, Cryosphere, Sea level rise, Physical geography, Precipitation, Outflow, Geology, Climate change