论文标题

夜间大气边界层和辐射雾中的穿透对流

Penetrative convection in nocturnal atmospheric boundary layer and radiation fog

论文作者

Kaushal, Shaurya, Singh, D. K., Sreenivas, K. R.

论文摘要

储层计算是预测湍流的有力工具,其简单的架构具有处理大型系统的计算效率。然而,其实现通常需要完整的状态向量测量和系统非线性知识。我们使用非线性投影函数将系统测量扩展到高维空间,然后将其输入到储层中以获得预测。我们展示了这种储层计算网络在时空混沌系统上的应用,该系统模拟了湍流的若干特征。我们表明,使用径向基函数作为非线性投影器,即使只有部分观测并且不知道控制方程,也能稳健地捕捉复杂的系统非线性。最后,我们表明,当测量稀疏、不完整且带有噪声,甚至控制方程变得不准确时,我们的网络仍然可以产生相当准确的预测,从而为实际湍流系统的无模型预测铺平了道路。

After the sunset, under calm and clear sky conditions, aerosol laden surface air-layer, cools radiatively to the upper atmosphere. Predominant effect of the radiative cooling on the vertical temperature profile extends to several hundred meters from the surface. This results in the development of a stable, nocturnal inversion layer. However, ground surface, owing to its higher thermal inertia, lags in the cooling process. Due to this about a meter thick air layer just above the ground can be (2-6)deg Celsius cooler than the ground. Thus, at the surface an unstable convective layer is present, which is capped by a stable inversion layer that extends up to several hundred meters. This configuration involving a convective mixed layer topped by a stably stratified inversion layer is a classic case of penetrative convection. Micrometeorological phenomenon at the surface, such as occurrence of fog, is determined by temperature profile, heat and moisture transport from the ground. Here, we present a computational study of the model penetrative convection, formed due to radiative cooling, in the nocturnal atmospheric boundary layer.

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