冰山分娩行为的变化在最后一次除冰期期间北海冰架解体之前发生
James D Kirkham1,2, Kelly A Hogan3, Robert D Larter3
1British Antarctic Survey, High Cross, Cambridge, UK. jamkir56@bas.ac.uk.
Nature communications
|April 24, 2025
概括
边缘英国-爱尔兰冰盖 (BIIS) 的冰架在18000年前解体. 这种向较小冰山的转变与冰盖的崩相吻合,可能是由表面融化和水力压裂引发的.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 地质形态学 地质形态学
背景情况:
- 冰架的稳定性对于南极冰盖 (AIS) 的支和海平面上升至关重要.
- 了解冰山分娩模式的变化对于预测冰架的行为和稳定性至关重要.
- 英国-爱尔兰冰盖 (BIIS) 历史提供了对过去冰架动态的见解.
研究的目的:
- 调查BIIS解体期间冰山分娩制度的变化.
- 为了确定BIIS冰架崩的时间和机制.
- 评估分娩模式转变对冰架稳定性和冰退的影响.
主要方法:
- 对埋藏的地形进行分析,以重建过去的冰架范围.
- 地质证据的年代测定,以确定冰架解体的时间表.
- 解读冰山大小的变化,以推断产卵周期的变化.
主要成果:
- 有证据表明BIIS边缘有大量的冰架.
- 大规模的表状冰山 (宽5-10公里,厚50-180米) 产生直到18000年前.
- 转向更小的冰山产量与广泛的冰架解体和海洋冰层崩相吻合.
结论:
- BIIS经历了大约18卡的气候值,导致其冰架的大规模表面融化.
- 裂的水力压裂可能引发了冰架的解体,并增加了冰的退缩速度.
- 产卵周期的变化会对冰架稳定性和冰盖动态产生重大影响.
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