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DOI | 10.1029/2020JD034162 |
Effects of Surface and Top Wind Shear on the Spatial Organization of Marine Stratocumulus-Topped Boundary Layers | |
Zamora Zapata M.; Heus T.; Kleissl J. | |
发表日期 | 2021 |
ISSN | 2169897X |
卷号 | 126期号:11 |
英文摘要 | The convective nature of Stratocumulus topped boundary layers (STBL) involves the motion of updrafts and downdrafts, driven by surface fluxes and radiative cooling, respectively. The balance between shear and buoyant forcings at the surface can determine the organization of updrafts between cellular and roll structures. We investigate the effect of varying shear at the surface and top of the STBL using Large Eddy Simulations, taking DYCOMS II RF01 as a base case. We focus on spatial identification of the following features: coherent updrafts and downdrafts, and observe how they are affected by varying shear. Stronger surface shear organizes the updrafts in rolls, causes less well-mixed thermodynamic profiles, and decreases cloud fraction and liquid water path (LWP). Stronger top shear also decreases cloud fraction and LWP more than surface shear, by thinning the cloud from the top. Features with stronger top than surface shear are associated with a net downward momentum transport and show early signs of decoupling. Classifying updrafts and downdrafts based on their vertical span and horizontal size confirms the dominance of tall objects spanning the whole STBL. Tall objects occupy 30% of the volume in the STBL, while short ones occupy less than 1%. For updraft and downdraft fluxes, these tall objects explain 65% of the vertical velocity variance and 83% of the buoyancy flux, on average. Stronger top shear also weakens the contribution of downdrafts to the turbulent fluxes and tilts the otherwise vertical development of updrafts. © 2021. American Geophysical Union. All Rights Reserved. |
英文关键词 | coherent structures; Spatial organization; Stratocumulus; Wind shear |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Atmospheres |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/185169 |
作者单位 | Department of Mechanical and Aerospace Engineering, University of California, San Diego, La Jolla, CA, United States; Department of Physics, Cleveland State University, Cleveland, OH, United States |
推荐引用方式 GB/T 7714 | Zamora Zapata M.,Heus T.,Kleissl J.. Effects of Surface and Top Wind Shear on the Spatial Organization of Marine Stratocumulus-Topped Boundary Layers[J],2021,126(11). |
APA | Zamora Zapata M.,Heus T.,&Kleissl J..(2021).Effects of Surface and Top Wind Shear on the Spatial Organization of Marine Stratocumulus-Topped Boundary Layers.Journal of Geophysical Research: Atmospheres,126(11). |
MLA | Zamora Zapata M.,et al."Effects of Surface and Top Wind Shear on the Spatial Organization of Marine Stratocumulus-Topped Boundary Layers".Journal of Geophysical Research: Atmospheres 126.11(2021). |
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