Effect of ocean surface waves on sea ice using coupled wave–ice–ocean modelling

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Shuo Li , Alexander Babanin , Qingxiang Liu , Jin Liu , Rui Li , Joey Voermans
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引用次数: 0

Abstract

The reduction of ice content in the context of climate change in polar oceans has sparked strong scientific interest in wave–ice interactions. To study the wave effect on sea ice in the marginal ice zone (MIZ), wave model WW3 and ocean–ice model MOM6-SIS2 are fully coupled by implementing schemes to account for non-breaking wave-induced turbulence and wave stress on ice. Improved estimations of ocean mixed layer depth and sea ice extent are achieved by incorporating the parameterizations of wave effects. The results also show that wave-induced turbulence enhances upper ocean mixing and significantly impedes ice growth with warmed sea surface in winter. Conversely, the sea surface is cooled in summer and the sea ice melt is slowed down. The wave stress on ice is predominantly directed towards the ice field and is comparable in magnitude to the wind stress. The sea ice extent is increased due to the wave stress.
利用波浪-冰-海洋耦合建模研究海洋表面波对海冰的影响
在气候变化的背景下,极地海洋冰含量的减少引发了对波冰相互作用的强烈科学兴趣。为了研究边缘冰区(MIZ)波浪对海冰的影响,波浪模型WW3和海冰模型MOM6-SIS2完全耦合,实现了考虑非破浪湍流和海冰波浪应力的方案。通过纳入波浪效应的参数化,改进了海洋混合层深度和海冰范围的估计。结果还表明,波浪引起的湍流增强了上层海洋的混合,并在冬季海面变暖时显著阻碍了冰的生长。相反,夏季海面变冷,海冰融化速度减慢。冰面上的波应力主要指向冰原,其强度与风应力相当。由于波浪应力的作用,海冰面积增大。
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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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