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首页> 外文期刊>Nonlinear processes in geophysics >Three-dimensional parameterizations of the synoptic scale kinetic energy and momentum flux in the Earth's atmosphere
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Three-dimensional parameterizations of the synoptic scale kinetic energy and momentum flux in the Earth's atmosphere

机译:地球大气中天气尺度动能和动量通量的三维参数化

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We present a new set of statistical-dynamical equations (SDEs) which can accurately reproduce the three-dimensional atmospheric fields of synoptic scale kinetic energy and momentum flux. The set of equations is closed by finding proper parameterizations for the vertical macro-turbulent diffusion coefficient and ageostrophic terms. The equations have been implemented in a new SD atmosphere model, named iAeolus/i. We show that the synoptic scale kinetic energy and momentum fluxes generated by the model are in good agreement with empirical data, which were derived from bandpass-filtered ERA-40 data. In addition to present-day climate, the model is tested for substantially colder (last glacial maximum) and warmer (2×COsub2/sub) climates, and shown to be in agreement with general circulation model (GCM) results. With the derived equations, one can efficiently study the position and strength of storm tracks under different climate scenarios with calculation time a fraction of those of GCMs. This work prepares ground for the development of a new generation of fast Earth System Models of Intermediate Complexity which are able to perform multi-millennia simulations in a reasonable time frame while appropriately accounting for the climatic effect of storm tracks.
机译:我们提出了一套新的统计-动力学方程(SDE),它可以准确地再现天气尺度动能和动量通量的三维大气场。通过为垂直宏观湍流扩散系数和年龄变迁项找到适当的参数化,可以关闭方程组。该方程已在名为 Aeolus 的新SD大气模型中实现。我们表明,该模型所产生的天气尺度动能和动量通量与从带通滤波后的ERA-40数据得出的经验数据高度吻合。除了当前的气候外,还对该模型进行了实质上更冷(最后一次冰川最大)和较暖(2×CO 2 )气候的测试,并证明与一般循环模型(GCM)一致结果。利用推导的方程式,可以有效地研究不同气候情景下风暴路径的位置和强度,而计算时间仅为GCM的一小部分。这项工作为开发新一代的中级复杂性快速地球系统模型奠定了基础,该模型能够在合理的时间范围内执行几千年的模拟,同时适当考虑了风暴轨迹的气候影响。

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