Parameterizing Heat and Moisture Exchange in a Regional Thermodynamic Model of Sea Ice

IF 16.4 1区 化学 Q1 CHEMISTRY, MULTIDISCIPLINARY Accounts of Chemical Research Pub Date : 2024-05-28 DOI:10.3103/s1068373924030038
D. D. Zav’yalov, T. A. Solomakha
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Abstract

The prevailing types of the atmospheric stratification over the snow-ice cover at the top of Taganrog Bay for eleven winter seasons of 2007/2008–2017/2018 have been determined using the numerical experiments on reproducing the seasonal variations in the sea ice thickness. Series of calculations both with the constant transfer coefficients and with the coefficients obtained taking into account the surface stratification of the atmosphere have been carried out. The model results of both series have been compared with each other and with in situ measurements.

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海冰区域热力学模型中的热量和水分交换参数化
摘要 利用再现海冰厚度季节性变化的数值实验,确定了 2007/2008-2017/2018 年十一个冬季塔甘罗格湾顶部雪冰覆盖层大气分层的主要类型。在恒定传递系数和考虑到大气表面分层的系数下进行了一系列计算。两个系列的模型结果已相互比较,并与现场测量结果进行了比较。
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来源期刊
Accounts of Chemical Research
Accounts of Chemical Research 化学-化学综合
CiteScore
31.40
自引率
1.10%
发文量
312
审稿时长
2 months
期刊介绍: Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance. Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.
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