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《新科学家》 第3596期 · 2026年5月23日 · 中文解读

末日冰川冰架即将崩解

'Doomsday' glacier on thin ice · Alison George
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南极洲最受威胁的思韦茨冰川的冰架即将脱离,其崩塌可能引发连锁反应,导致全球海平面上升3.3米。
原文开头
‘Doomsday’ glacier on thin ice The ice shelf holding back Thwaites glacier in Antarctica is starting to break up, with worrying implications for global sea levels, finds Alison George ANTARCTICA’S most threatened glacier is about be further destabilised, as the floating ice shelf in front of Thwaites glacier is set to detach. Dubbed the “doomsday glacier”, Thwaites is about the size of Britain, but it is shrinking rapidly and is already responsible for 4 per cent of all global sea-level rise. Worse still, its collapse is expected to set off a domino effect in the entire West Antarctic ice sheet, ultimately resulting in a calamitous sea-level rise of 3.3 metres and changing the coastline of the entire planet. …
摘自《新科学家》(New Scientist)第3596期 · 2026年5月23日,Alison George。仅引用开头一小段供了解文章,版权归原刊所有,全文请阅读原刊。
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