冰川
冰消
气候变化
海平面上升
全球变暖
全球变化
气候学
环境科学
自然地理学
海平面
纬度
大气科学
地质学
冰期
海洋学
地理
地貌学
大地测量学
作者
David R. Rounce,Regine Hock,Fabien Maussion,Romain Hugonnet,William Kochtitzky,Matthias Huss,Étienne Berthier,Douglas Brinkerhoff,Loris Compagno,Luke Copland,Daniel Farinotti,Brian Menounos,Robert McNabb
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2023-01-05
卷期号:379 (6627): 78-83
被引量:266
标识
DOI:10.1126/science.abo1324
摘要
Glacier mass loss affects sea level rise, water resources, and natural hazards. We present global glacier projections, excluding the ice sheets, for shared socioeconomic pathways calibrated with data for each glacier. Glaciers are projected to lose 26 ± 6% (+1.5°C) to 41 ± 11% (+4°C) of their mass by 2100, relative to 2015, for global temperature change scenarios. This corresponds to 90 ± 26 to 154 ± 44 millimeters sea level equivalent and will cause 49 ± 9 to 83 ± 7% of glaciers to disappear. Mass loss is linearly related to temperature increase and thus reductions in temperature increase reduce mass loss. Based on climate pledges from the Conference of the Parties (COP26), global mean temperature is projected to increase by +2.7°C, which would lead to a sea level contribution of 115 ± 40 millimeters and cause widespread deglaciation in most mid-latitude regions by 2100.
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