冰面阻断海洋热量传输到南极冰架
A K Wåhlin1, N Steiger2,3, E Darelius2,3
1Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden. awahlin@gu.se.
Nature
|February 28, 2020
概括
南极的冰架正在由于海洋升温而融化. 一个类似阶梯的冰面阻断了热流,限制了融化和冰的损失. 这一发现对于气候模型至关重要.
科学领域:
- 海洋学
- 冰川学
- 气候科学
背景情况:
- 南极冰层的质量损失正在加速.
- 冰架的基础融化推动了这一变化.
- 海洋热传输到大陆架是一个关键重点.
研究的目的:
- 调查海洋热传输到南极冰架的控制.
- 确定为什么向岸的热量流超过观察到的融化速率.
- 了解冰面地形在调节热流中的作用.
主要方法:
- 从盖茨冰架进行直接观测.
- 在旋转平台上的实验室实验.
- 热流组件的分析 (巴罗热和巴罗临床).
主要成果:
- 阶梯形的冰面阻断了独立于深度的热流.
- 只有较小,深度不同 (巴洛克林) 的热成分进入冰下腔.
- 这种阻断机制解释了热量流和融化速率之间的差异.
结论:
- 冰面地形是控制海洋热量进入冰架下空洞的关键因素.
- 在模拟融化速率时,必须准确地呈现冰的前层地形.
- 这一发现可能解释了为什么水柱密度的变化比棚式热传输更能表明变性.
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