Floes, the marginal ice zone and coupled wave-sea-ice feedbacks.

Floes, the marginal ice zone and coupled wave-sea-ice feedbacks.
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DOI:
10.1098/rsta.2021.0252
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发表时间:
2022-10-31
影响因子:
5
通讯作者:
Horvat, Christopher
Horvat, Christopher
中科院分区:
综合性期刊2区
文献类型:
--
作者:
Horvat, Christopher

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边缘冰区(MIZ)是性质独特的海冰覆盖区域,在极地海洋与更广泛的地球系统之间的相互作用中发挥着关键作用。 MIZ 区域的海洋、大气和生态条件具有较高的时空变化性。 MIZ 的显着质量特征是它们由单个浮冰镶嵌而成,水平范围从厘米到数十公里不等。因此,絮凝物尺寸分布(FSD)可用于定量识别和描述它们。本文回顾了 FSD 观测和理论的历史,以及决定浮冰尺寸和尺寸分布的过程(特别是海浪的影响)。使用 MIZ 中热力学波-海冰相互作用的随机模型探索耦合波-FSD 反馈,并讨论了这个快速发展领域中的一些关键的开放问题。本文是主题“边缘冰区动力学的理论、建模和观察:多学科视角和展望”的一部分。
Marginal ice zones (MIZs) are qualitatively distinct sea-ice-covered areas that play a critical role in the interaction between the polar oceans and the broader Earth system. MIZ regions have high spatial and temporal variability in oceanic, atmospheric and ecological conditions. The salient qualitative feature of MIZs is their composition as a mosaic of individual floes that range in horizontal extent from centimetres to tens of kilometres. Thus the floe size distribution (FSD) can be used to quantitatively identify and describe them. Here, the history of FSD observations and theory, and the processes (particularly the impact of ocean waves) that determine floe sizes and size distribution, are reviewed. Coupled wave-FSD feedbacks are explored using a stochastic model for thermodynamic wave-sea-ice interactions in the MIZ, and some of the key open questions in this rapidly growing field are discussed. This article is part of the theme issue ‘Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks’.
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