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《新科学家》 2026年9月26日 · 中文解读

海洋告急:关键洋流濒临崩溃

Trouble at sea · Alec Luhn
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格陵兰东南部索根弗里冰川附近,一座长达1公里的冰墙崩塌入峡湾,约1800万吨冰体倾覆。冰崩正削弱对欧洲至关重要的北大西洋经向翻转环流(AMOC),一旦停摆,欧洲将陷入“冰期”寒冬与常年干旱。英国科研机构正推进一项8100万英镑计划,试图建立AMOC临界点的早期预警系统。
原文开头
A crucial ocean current is at risk of shutting down. How close is this disaster and what happens next, asks Alec Luhn On a sunny evening in July, a research ship called the Sir David Attenborough was working near the Sorgenfri glacier in south-eastern Greenland when a kilometre-long wall of craggy, bulging ice collapsed into the fjord. The scientists on deck watched in stunned silence as an estimated 18 million tonnes of ice slowly flipped over, sending up vast plumes of spray. Iceberg calving on this scale was once relatively rare – but it has become commonplace in recent years as Earth warms. And that acceleration could have catastrophic impacts that extend far beyond Greenland. …
摘自《新科学家》(New Scientist)2026年9月26日,Alec Luhn。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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