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风暴引起的海冰破裂以及对冰面范围的影响
A L Kohout1, M J M Williams2, S M Dean2
1National Institute of Water and Atmospheric Research, Christchurch 8011, New Zealand.
Nature
|May 30, 2014
概括
大海浪在距离冰边数百公里的南极海冰上破裂,挑战了以前的模型. 这一发现揭示了波浪能量在海冰解体和撤退动态中的重要作用.
科学领域:
- 海洋学 海洋学 海洋学
- 冰川学的冰川学
- 气候科学 气候科学
背景情况:
- 了解海冰解体对于预测北极和南极变化至关重要.
- 之前的研究缺乏通过海冰传播的大型风暴产生的波的直接测量.
研究的目的:
- 测量风暴产生的海洋波对南极海冰的影响.
- 为了研究由海洋波引起的海冰破裂的机制和程度.
主要方法:
- 在南极海冰的多个位置同时进行观测.
- 对不同波浪大小的波浪高度衰减 (线性与指数) 的分析.
- 观察到的海冰边缘位置与模拟的显著波高度的比较.
主要成果:
- 大型海洋波浪 (显著的波浪高度>3米) 打破海冰远远的内陆比预测.
- 波高衰变对于大波来说几乎是线性的,而不是通常认为的指数式.
- 海冰边缘的撤退和扩张与海浪高度的分别增加和减少有关.
结论:
- 大海浪在海冰的破裂和退缩中扮演的角色比以前理解的要重要得多.
- 当前的气候模型可能需要纳入波冰相互作用,以准确预测海冰变化.
- 这些发现为改善海冰和气候模型提供了关键数据.
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