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Updated: Feb 27, 2026

Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
西南极冰盖的退缩是由热水入侵驱动的
Claus-Dieter Hillenbrand1, James A Smith1, David A Hodell2
1British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK.
温暖的环极深水 (CDW) 侵袭融化了南极西部的冰架,导致冰盖退缩. 全新纪数据显示,与风力转移相关的CDW上升导致了阿蒙森海的过去和最近的脱冰.
科学领域:
- 古气候学和冰川学:研究过去的气候动态及其对冰盖稳定性的影响.
背景情况:
- 西南极冰层 (WAIS) 容易受到海洋驱动的融化影响.
- * 环极深水 (CDW) 侵袭大陆架导致基底冰架融化.
- * 冰架变薄会减少支,加速冰川流动和冰盖的退缩.
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