T. Waterman, A. D. Bragg, F. Hay-Chapman, P. A. Dirmeyer, M. D. Fowler, J. Simon, N. Chaney
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引用次数: 0
Abstract
Earth system models currently struggle to account for the complex effects that land surface heterogeneity can have on land-atmosphere interactions. There have been attempts to include the impact of this heterogeneity on the atmosphere, but they ignore the development of coherent circulations that can be driven by spatial differential surface heating. A wealth of literature, particularly large-eddy simulation (LES) based studies, shows that these circulations have significant impacts on the development and organization of clouds. In this work, we describe a two-column model with a parameterized circulation driven by atmospheric virtual potential temperature profiles, differences in near surface temperature between the two columns, patterns of surface heterogeneity, and the mean background wind. Key aspects of the proposed model structure are compared with LES output, and the model is then implemented between two otherwise independent single column models. While some avenues for improvement exist, when the circulations are parameterized, we see increased cloud development and realistic changes to the mean profiles of temperature and moisture. The proposed model qualitatively matches expectations from the literature and LES, and points to the potential success of its future implementation in coarse grid models.
目前,地球系统模式很难解释地表异质性对陆地-大气相互作用的复杂影响。有人曾尝试将这种异质性对大气的影响包括在内,但却忽略了空间差异表面加热可能驱动的相干环流的发展。大量文献,特别是基于大涡模拟(LES)的研究表明,这些环流对云的发展和组织有重大影响。在这项工作中,我们描述了一个双柱模型,该模型的参数化环流由大气虚拟势温度剖面、双柱之间的近表面温度差异、表面异质性模式和平均背景风驱动。建议的模式结构的关键方面与 LES 输出进行了比较,然后在两个原本独立的单柱模式之间实施了该模式。虽然还存在一些需要改进的地方,但当环流参数化后,我们看到云层发展增加了,温度和湿度的平均剖面也发生了现实的变化。所提出的模型在质量上符合文献和 LES 的预期,并预示着未来在粗网格模型中实施该模型可能会取得成功。
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