Articles | Volume 17, issue 11
https://doi.org/10.5194/acp-17-6547-2017
https://doi.org/10.5194/acp-17-6547-2017
Research article
 | 
02 Jun 2017
Research article |  | 02 Jun 2017

Glacier evolution in high-mountain Asia under stratospheric sulfate aerosol injection geoengineering

Liyun Zhao, Yi Yang, Wei Cheng, Duoying Ji, and John C. Moore

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Cited articles

Applegate, P. J. and Keller, K.: How effective is albedo modification (solar radiation management geoengineering) in preventing sea-level rise from the Greenland Ice Sheet?, Environ. Res. Lett., 10, 084018, https://doi.org/10.1088/1748-9326/10/8/084018, 2015.
Arora, V. K., Scinocca, J. F., Boer, G. J., Christian, J. R., Denman, K. L., Flato, G. M., Kharin, V. V., Lee, W. G., and Merryfield, W. J.: Carbon emission limits required to satisfy future representative concentration pathways of greenhouse gases, Geophys. Res. Lett., 38, L05805, https://doi.org/10.1029/2010GL046270, 2011.
Azam, M. F., Wagnon, P., Ramanathan, A., Vincent, C., Sharma, P., Arnaud, Y., Linda, A., Pottakkal, G. J., Chevallier, P., Singh, V. B., and Berthier, E.: From balance to imbalance: a shift in the dynamic behaviour of Chhota Shigri Glacier (Western Himalaya, India), J. Glaciol., 58, 315–324, 2012.
Bahr, D. B., Meier, M., and Peckham, S.: The physical basis of glacier volume–area scaling, J. Geophys. Res., 102, 355–362, 1997.
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Short summary
We find stratospheric sulfate aerosol injection geoengineering, G3, can slow shrinkage of high-mountain Asia glaciers by about 50 % by 2069 relative to losses from RCP8.5. The reduction in mean precipitation expected for solar geoengineering is less important than the temperature-driven shift from solid to liquid precipitation for forcing Himalayan glacier change. The termination of geoengineering in 2069 leads to temperature rise of 1.3 °C and corresponding increase in glacier volume loss rate.
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