Initial estimate of the contribution of cryospheric change in China to sea level rise

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Abstract

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. © 2011 The Author(s).

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Ren, J. W., Ye, B. S., Ding, Y. J., & Liu, S. Y. (2011). Initial estimate of the contribution of cryospheric change in China to sea level rise. Chinese Science Bulletin, 56(16), 1661–1664. https://doi.org/10.1007/s11434-011-4474-3

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