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Article | Publishing Language: Chinese

Impact of PBL eddy transport on the 20 July 2021 Zhengzhou torrential rainfall

Chengzhi YE1,2Rui CHENG3Zejun DAI1,4Yang WANG3Jingjing CHEN1,4Zhenzhen WU1,2
Hunan Key Laboratory of Meteorological Disaster Prevention and Reduction, Changsha 410118, China
Hunan Institute of Meteorological Science, Changsha 410118, China
State Key Laboratory of Geo-Information Engineering, Xi'an 710054, China
Hunan Meteorological Observatory, Changsha 410118, China
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Abstract

The "7.20" Zhengzhou torrential rainfall is the most severe storm in the 21st century, characterized by long persistence and intense hourly precipitation. Through comparative analysis of PBL (Planetary Boundary Layer) eddy transport for this instantaneous precipitation process, this study attempts to investigate PBL structure and turbulent diffusion impacts on heavy precipitation intensity. Three comparative experiments are conducted by tuning coefficients of local eddy diffusion and counter-gradient term. Results show that PBL turbulent transport has strong influences on severe hourly precipitation during the "7.20" Zhengzhou torrential rainfall event. It is found through comparison that the decrease in local eddy diffusion noticeably leads to weakening in precipitation intensity and the counter-gradient term mainly results in changes in rainfall location and evolution. Furthermore, PBL eddy transport can modulate large-scale atmospheric conditions for heavy storms, such as local water vapor supply and atmospheric instability. Finally, the eddy vapor and heat transports can notably modify the distribution, intensity and evolution of moisture flux convergence and PBL atmospheric instability, and thus exhibit great influences on this severe storm simulation.

CLC number: P426.6 Document code: A

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Acta Meteorologica Sinica
Pages 1258-1270

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Cite this article:
YE C, CHENG R, DAI Z, et al. Impact of PBL eddy transport on the 20 July 2021 Zhengzhou torrential rainfall. Acta Meteorologica Sinica, 2025, 83(5): 1258-1270. https://doi.org/10.11676/qxxb2025.20240051

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Received: 18 April 2024
Revised: 12 February 2025
Published: 28 October 2025
Copyright © 2025 Acta Meteorologica Sinica. All rights reserved.