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首页> 外文期刊>Boundary-layer Meteorology >Amendment to 'Analytical Solution for the Convectively-Mixed Atmospheric Boundary Layer': Inclusion of Subsidence
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Amendment to 'Analytical Solution for the Convectively-Mixed Atmospheric Boundary Layer': Inclusion of Subsidence

机译:对“对流混合大气边界层的解析解”的修正:包括沉降

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In Ouwersloot and Vila-Guerau de Arellano (Boundary-Layer Meteorol. doi: 10. 1007/s10546-013-9816-z, 2013, this issue), the analytical solutions for the boundary-layer height and scalar evolutions are derived for the convective boundary layer, based on the prognostic equations of mixed-layer slab models without taking subsidence into account. Here, we include and quantify the added effect of subsidence if the subsidence velocity scales linearly with height throughout the atmosphere. This enables analytical analyses for a wider range of observational cases. As a demonstration, the sensitivity of the boundary-layer height and the potential temperature jump to subsidence and the free tropospheric stability is graphically presented. The new relations show the importance of the temporal distribution of the surface buoyancy flux in determining the evolution if there is subsidence.
机译:在Ouwersloot和Vila-Guerau de Arellano(边界层Meteorol。doi:10。1007 / s10546-013-9816-z,2013年,本期)中,得出了边界层高度和标量演化的解析解。对流边界层,基于混合层板模型的预测方程,不考虑沉降。在这里,如果沉降速度与整个大气层的高度成线性比例关系,那么我们将包括并量化沉降的附加影响。这样就可以对更广泛的观察案例进行分析。作为演示,边界层高度的敏感性和潜在的温度跃迁到沉降和自由对流层稳定性的图形表示。新的关系表明,如果存在沉陷,则表面浮力通量的时间分布对于确定演化的重要性。

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