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当代边缘冰区研究的预测性概述。

A prognosticative synopsis of contemporary marginal ice zone research.

机构信息

Department of Mathematics and Statistics, University of Otago, PO Box 56, Dunedin 9016, New Zealand.

出版信息

Philos Trans A Math Phys Eng Sci. 2022 Oct 31;380(2235):20220094. doi: 10.1098/rsta.2022.0094. Epub 2022 Sep 12.

Abstract

Commentary narrated in this theme issue is recast to contextualize the diverse themes presented into a forward-looking conversation that synthesizes, debates opportunities for multidisciplinary advances and highlights topics that deserve enduring sharpened attention. Research oriented towards foundational elements of the marginal ice zone that relates to three unifying topic subclasses-namely (i) wave propagation through sea ice, (ii) floe size distributions and (iii) ice dynamics and break-up-and is encapsulated in mini-reviews provided by Thomson, Horvat and Dumont is revisited to distill it into a blueprint for the future guided by the cutting-edge, present-day knowledge documented herein by leading practitioners in the field. Six threads are signalled as imperative for prospective research, each with a bearing on Arctic and Antarctic sea-ice canopies in which the propensity for marginal ice zones to coexist with pack ice is greater as a result of global climate change reducing sea-ice resilience while increasing the prevalence and forcefulness of injurious storm winds and waves. This article is part of the theme issue 'Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks'.

摘要

本主题特刊中的评论叙述被重新构建,以便将呈现的各种主题纳入前瞻性对话中,综合、辩论多学科进展的机会,并突出值得持久关注的主题。以与三个统一的主题子类相关的边缘冰区的基础要素为研究方向——即 (i) 波在海冰中的传播、(ii) 浮冰块大小分布和 (iii) 冰动力学和破裂——并封装在由 Thomson、Horvat 和 Dumont 提供的迷你评论中,以将其提炼为未来蓝图,由该领域的领先从业者在此处记录的前沿、当今知识指导。有六个线索被标记为未来研究的必要条件,每个线索都与北极和南极海冰的覆盖层有关,由于全球气候变化降低了海冰的弹性,同时增加了破坏性风暴风和波浪的普遍性和强度,边缘冰区与浮冰共存的趋势更大。本文是特刊“边缘冰区动力学的理论、建模和观测:多学科视角和展望”的一部分。

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