南极海冰的驱动者越来越多
Kenza Himmich1, Martin Vancoppenolle2, Gurvan Madec2,3
1Sorbonne Université, Laboratoire d'Océanographie et du Climat, CNRS/IRD/MNHN, Paris, France. kenza.himmich@locean.ipsl.fr.
Nature communications
|October 5, 2023
概括
南极海冰的前进是由一些地区的结和其他地区的冰进口驱动的. 海冰退缩和海洋热量储存的时间强烈影响海冰季节的开始.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 冰层科学 冰层科学 冰层科学
背景情况:
- 南极海冰主要是季节性的,近几十年来观察到它的季节性变化.
- 缺乏对过程的理解,阻碍了对这些观察到的海冰季节性变化的解释.
- 研究海冰季节开始 (提前) 的驱动因素对于了解季节性海冰动态至关重要.
研究的目的:
- 为了研究推动南极海冰前进的物理过程.
- 区分季节性冰区不同区域的海冰前进机制.
- 了解海冰前进,后退和海洋热特性之间的关系.
主要方法:
- 利用遥感数据进行大规模观测.
- 使用现场观察来进行详细的过程分析.
- 分析了海冰前进时间和海洋混合层热量含量之间的关系.
主要成果:
- 海水结是海冰在内部季节性冰区前进的主要驱动因素.
- 在季节性冰区的外部带,海冰的前进是由漂流冰进口到更温暖的水域驱动的.
- 海冰的前进日期与夏季海洋混合层储存的热量密切相关.
- 海冰退缩的时间决定了夏季海洋混合层的热量含量,在退缩和提前日期之间建立了联系.
结论:
- 海冰退缩和前进之间的热力学联系,由海洋储热介导,显著限制季节性海冰气候学.
- 虽然这种联系影响年际变化,但与气候学约束相比,其影响不那么明显.
- 了解这些独特的进步机制对于预测未来南极海冰的行为至关重要.
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