Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi

Based on multiscale diagnosis method of energy budget, the missing-forecast coastal warm-sector rainstorm process of Guangxi occurred in 24-26 January 2020 was analyzed by using the stational data, Doppler radar, FY-2G satellite data and the ERA5 reanalysis data. The results are shown below: The war...

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Main Authors: Hao QIN, Zhiyi WANG, Yinning SHI, Shunan ZHAI, Liyan QI
Format: Article
Language:zho
Published: Editorial Office of Torrential Rain and Disasters 2023-06-01
Series:暴雨灾害
Subjects:
Online Access:http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2022-094
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author Hao QIN
Zhiyi WANG
Yinning SHI
Shunan ZHAI
Liyan QI
author_facet Hao QIN
Zhiyi WANG
Yinning SHI
Shunan ZHAI
Liyan QI
author_sort Hao QIN
collection DOAJ
description Based on multiscale diagnosis method of energy budget, the missing-forecast coastal warm-sector rainstorm process of Guangxi occurred in 24-26 January 2020 was analyzed by using the stational data, Doppler radar, FY-2G satellite data and the ERA5 reanalysis data. The results are shown below: The warm and moisture southwest jet in front of the southern branch trough provides a favorable synoptic condition for the rainstorm. The convection system was constantly triggered by the trumpet topography in the northeast of Vietnam, and moved northeastward to the coastal of Guangxi, which was influenced by the upper level airflow and produced significant amount of precipitation. It is found that the occurrence and development of warm-sector rainstorm were mainly dominated by the convection-scale kinetic energy that correlated well with the former in evolution. The convective energy mainly come from the middle and lower troposphere and losts in the upper troposphere. The kinetic energy from the background scale contributed the most, and the barotropic instability of the background flow field in the middle and lower troposphere dominated the development of rainstorm in the warm-sector. The buoyancy conversion of convection-scale available potential energy to kinetic energy in the middle troposphere further promoted the development of system. The transport of kinetic energy made the convection-scale kinetic energy distribute evenly spatially, which led to the stable development of the convective system and enabled it to maintain for long time and thus produce large amount of precipitation over its path. The contribution of synoptic-scale kinetic energy conversion and pressure gradient work is small, which reflects the nature of weak synoptic-scale forcing of warm-sector rainstorm.
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spelling doaj.art-a732aefa863c4efd914b23778de267302023-07-12T10:56:04ZzhoEditorial Office of Torrential Rain and Disasters暴雨灾害2097-21642023-06-0142328329210.12406/byzh.2022-094byzh-42-3-283Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of GuangxiHao QIN0Zhiyi WANG1Yinning SHI2Shunan ZHAI3Liyan QI4Guangxi Meteorological Observatory, Nanning 530022China Meteorological Administration Economic Transformation of Climate Resources Key Laboratory, Chongqing Meteorological Observatory, Chongqing 401147CMA Earth System Modeling and Prediction Centre, Beijing 100081Guangxi Meteorological Observatory, Nanning 530022Guangxi Meteorological Observatory, Nanning 530022Based on multiscale diagnosis method of energy budget, the missing-forecast coastal warm-sector rainstorm process of Guangxi occurred in 24-26 January 2020 was analyzed by using the stational data, Doppler radar, FY-2G satellite data and the ERA5 reanalysis data. The results are shown below: The warm and moisture southwest jet in front of the southern branch trough provides a favorable synoptic condition for the rainstorm. The convection system was constantly triggered by the trumpet topography in the northeast of Vietnam, and moved northeastward to the coastal of Guangxi, which was influenced by the upper level airflow and produced significant amount of precipitation. It is found that the occurrence and development of warm-sector rainstorm were mainly dominated by the convection-scale kinetic energy that correlated well with the former in evolution. The convective energy mainly come from the middle and lower troposphere and losts in the upper troposphere. The kinetic energy from the background scale contributed the most, and the barotropic instability of the background flow field in the middle and lower troposphere dominated the development of rainstorm in the warm-sector. The buoyancy conversion of convection-scale available potential energy to kinetic energy in the middle troposphere further promoted the development of system. The transport of kinetic energy made the convection-scale kinetic energy distribute evenly spatially, which led to the stable development of the convective system and enabled it to maintain for long time and thus produce large amount of precipitation over its path. The contribution of synoptic-scale kinetic energy conversion and pressure gradient work is small, which reflects the nature of weak synoptic-scale forcing of warm-sector rainstorm.http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2022-094warm-sector rainstormmultiscale window transformcanonical transferbarotropic instabilityconvection energy
spellingShingle Hao QIN
Zhiyi WANG
Yinning SHI
Shunan ZHAI
Liyan QI
Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
暴雨灾害
warm-sector rainstorm
multiscale window transform
canonical transfer
barotropic instability
convection energy
title Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
title_full Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
title_fullStr Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
title_full_unstemmed Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
title_short Multiscale diagnosis of the energy budget for a warm-sector rainstorm event in winter in the coastal area of Guangxi
title_sort multiscale diagnosis of the energy budget for a warm sector rainstorm event in winter in the coastal area of guangxi
topic warm-sector rainstorm
multiscale window transform
canonical transfer
barotropic instability
convection energy
url http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2022-094
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