The numerical simulations are conducted with the coupled general circulation model for various lengths of the annual cycle. The modeling results confirm a previous conclusion, which is based on analysis of climate data using a special method of amplitude phase characteristics, that the thickness of the troposphere (the height of the tropopause) corresponds to the height of the temperature skin layer for the atmosphere under periodic heating from the surface related with the annual insolation cycle. In particular, the model height of the tropopause for half of the duration of the annual cycle is lower by \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\sqrt 2 $$\end{document} in comparison with the present-day length of the annual cycle.

中文翻译：

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大气垂直温度分层取决于耦合环流模型模拟的年日照周期长度

数值模拟是用耦合环流模型对不同长度的年循环进行的。建模结果证实了之前的结论，该结论基于使用特殊的振幅相位特征方法对气候数据进行分析，即对流层的厚度（对流层顶的高度）对应于大气温度表层的高度。在与年度日照周期相关的地表周期性加热下。特别是，