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The turbulent kinetic energy budget for shallow cumulus convection

机译:浅积云对流的湍动能预算

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摘要

Turbulence Kinetic Energy (TKEl budgets derived from large-eddy simulations of the cumulus-aipped boundary layer are analysed using recently developed similarity ideas. The budgets for the main part of the cumulus layer and the overlying inversion andthe cloud-base transition zone are considered separately. The terms in the budget can be sealed using the similarity theory developed by Grant and Brown (1999). Below the inversion, TKE is produced by buoyancy, with the transport of TKE representing a loss of TKE. In the inversion layer, the transport of TKE from the underlying cloud layer is the dominant production term, although negatively buoyant downdraughts are present in the upper part of the inversion and contribute to the production of TKR. Theterms in the TKE budget in the transition zone between the subcloud and cloud layers scale with mixed-layer scales, but for the buoyancy production term there is a region in which both mixed-layer and cloud-layer scalings are valid. Using the mass-fluxapproximation in conjunction with the scaling results, it is shown that it is possible to obtain a parametrization of the cumulus mass-flux profile.
机译:湍流动能(TKEl预算)是使用最近开发的相似性思想对源自积云边界层的大涡模拟进行分析的。积云层主要部分的预算以及上覆的反演和云基过渡带分别考虑可以使用Grant和Brown(1999)提出的相似性理论来密封预算中的各项;在反演之下,TKE是由浮力产生的,TKE的运输代表了TKE的损失。来自底层云层的TKE的数量是主要的生产术语,尽管反演的上部存在负浮力下沉气流,并且有助于TKR的产生。对于混合层尺度,但对于浮力生产而言,存在一个区域,其中混合层和云层尺度均有效。质量通量近似与定标结果相结合,表明可以对积质量通量分布进行参数化。

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