Vertical temperature in the atmoshere during surface inversions

机译：表面反转期间大气中的垂直温度

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In this article we present a mathematical model for the surface inversion in the meteorology and propose a numerical method which is based on the finite difference approximation and the Schwartz distribution. Through our discussion, a numerical simulation which is characterized by the inversion of the temperature gradient is presented.

机译：在本文中，我们提出了一种用于气象学中地表反演的数学模型，并提出了一种基于有限差分近似和Schwartz分布的数值方法。通过我们的讨论，提出了以温度梯度反演为特征的数值模拟。

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来源
《Advances in Computational Methods in Sciences and Engineering 2005 vol.4A; Lecture Series on Computer and Computational Sciences; vol.4A》|2005年|288-291|共4页
会议地点 Loutraki(GR)
作者
H. Koshigoe; T. Shiraishi; M. Ehara;
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作者单位

Department of Urban Environment Systems, Faculty of Engineering, Chiba University, 263-8522, Chiba, Japan;

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会议组织
原文格式 PDF
正文语种 eng
中图分类计算数学的应用;
关键词
direct method; schwartz distribution; surface inversion;

机译：直接法施华兹分布;表面反演;

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机译：曲面的垂直和水平反转
4. Vertical temperature in the atmoshere during surface inversions [C] . H. Koshigoe, T. Shiraishi, M. Ehara Advances in Computational Methods in Sciences and Engineering 2005 vol.4A; Lecture Series on Computer and Computational Sciences; vol.4A . 2005

机译：表面反转期间大气中的垂直温度
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7. Heat-Transfer from a Vertical Flat Surface by Laminar Free-Convection : The cases where the physical constants of fluids depend on the temperatures and the surface has an arbitrary temperature distribution in vertical direction [O] . Tetsu FUJII 1958

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Vertical temperature in the atmoshere during surface inversions

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