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Numerical study of the impact of the changes in the tropospheric temperature profile on the microphysics, dynamics and precipitation of mid-latitude summer continental convective clouds

机译:对流层温度剖面变化对中纬度夏季大陆对流云微物理,动力学和降水影响的数值研究

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摘要

This paper investigates the effect of the expected changes of tropospheric temperature profile on the dynamical and microphysical characteristics of individual summertime convective storms and on the processes of precipitation development in these storms. Two dynamically different clouds (a 'big' and a 'small' one) were simulated with the Regional Atmospheric Modeling System (RAMS v6.0). The differences between simulations of the clouds, developed in a present-day and in a modified environment are discussed. Macro- and microphysical evolution is examined in detail, and the changes in precipitation intensity and total rainfall volume are explained physically as a consequence of the temperature increase in the upper troposphere. Results show that the warming leads to a decrease of precipitation in the 'small' cloud case, while in the 'big' cloud case, warming leads to the increase of precipitation. The detailed analysis reveals that the main reason for the opposite direction of the impact of the projected tropospheric changes on different sized clouds lies in the ice phase evolution.
机译:本文研究了对流层温度剖面的预期变化对单个夏季对流风暴的动力学和微物理特征以及这些风暴中降水形成过程的影响。使用区域大气建模系统(RAMS v6.0)模拟了两个动态不同的云(“大”和“小”)。讨论了在当今和修改后的环境中开发的云模拟之间的差异。详细检查了宏观和微观物理演变,并通过对流层上层温度升高的结果,从物理上解释了降水强度和总降水量的变化。结果表明,在“小”云情况下,变暖导致降水减少,而在“大”云情况下,变暖导致降水增加。详细的分析表明,对流层变化的预测对不同大小的云的影响方向相反的主要原因在于冰期的演变。

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