解释了韦德尔波利尼亚 - - 在莫德起处的一个大型海洋旋棚
1Center for Atmosphere-Ocean Science, Courant Institute of Mathematical Sciences and Faculty of Arts and Science, New York University, New York, NY 10012, USA. holland@cims.nyu.edu
概括
韦德尔波利尼亚 (Weddell Polynya) 是南极海冰中的一个大开口,由海洋流与莫德海拔海山相互作用引起的. 这种相互作用会产生旋,打开冰,大气变化加剧了这种效应.
科学领域:
- 海洋学 海洋学 海洋学
- 海冰物理学 海洋冰物理学
- 南极气候动力学 南极气候动力学
背景情况:
- 韦德尔波利尼亚是通过卫星观察到的南极海冰中经常出现的大开口.
- 它的短暂性质和特殊特征并没有被以前的机制完全解释.
研究的目的:
- 阐明负责形成的物理机制,位置,大小和形状的韦德尔多林亚.
- 通过结合的海冰海洋计算机模型验证拟议的机制.
主要方法:
- 对韦德尔波利尼亚的卫星观测结果的分析.
- 理论上的解释涉及海洋流经过莫德起海山.
- 使用结合的海冰海洋模型进行数值模拟.
主要成果:
- 经过毛德海峡的大规模海洋流的适度变化会产生旋风.
- 棚引发了不同的Ekman应力,在海冰中创造了一个半月形的开口.
- 大气相互作用通过触发海洋对流来增强多.
结论:
- 拟议的机制是由毛德升起的海洋旋所驱动的,完全解释了韦德尔波利尼亚事件.
- 海洋动态,海冰和大气之间的相互作用对多形成至关重要.
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