Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China

Abstract This article aims to examine the diurnal variation of heavy rainfall (HR) for various intensities and investigate duration and environment of HR during the warm season over South China. Results show that the HR mainly occurred in the late afternoon over most regions of Guangdong Province (G...

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Main Author: Shui‐xin Zhong
Format: Article
Language:English
Published: Wiley 2020-06-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.969
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spelling doaj-9b6409f6558d4ca7a5db15307d7584322020-11-25T02:56:08ZengWileyAtmospheric Science Letters1530-261X2020-06-01216n/an/a10.1002/asl.969Diurnal variation of the duration and environment for heavy rainfall during the warm season in South ChinaShui‐xin Zhong0Guangdong Province Key Laboratory of Regional Numerical Weather Prediction Institute of Tropical and Marine Meteorology, CMA Guangzhou ChinaAbstract This article aims to examine the diurnal variation of heavy rainfall (HR) for various intensities and investigate duration and environment of HR during the warm season over South China. Results show that the HR mainly occurred in the late afternoon over most regions of Guangdong Province (GD) and east of Guangxi Province (GX), as well as the nocturnal‐to‐morning rainfall over the mountainous regions of northwestern GX and contiguous regions among GD. It exhibited two diurnal peaks in the early morning and in the late afternoon. HR which mostly occurred during the late afternoon by 1,700–1,900 LST exhibited longer durations (3–4 hr). The enhanced southerly wind and northerly wind over the mountainous, as well as the enhancement associated with strong horizontal surface‐temperature gradient due to surface heating and stronger vertical wind shear in the lower troposphere, contributed to the high‐frequency occurrences of the rainfall in the late afternoon.https://doi.org/10.1002/asl.969atmospheregeophysical sphereobservational data analysisphysical phenomenonrainfallseasonal scale
collection DOAJ
language English
format Article
sources DOAJ
author Shui‐xin Zhong
spellingShingle Shui‐xin Zhong
Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
Atmospheric Science Letters
atmosphere
geophysical sphere
observational data analysis
physical phenomenon
rainfall
seasonal scale
author_facet Shui‐xin Zhong
author_sort Shui‐xin Zhong
title Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
title_short Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
title_full Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
title_fullStr Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
title_full_unstemmed Diurnal variation of the duration and environment for heavy rainfall during the warm season in South China
title_sort diurnal variation of the duration and environment for heavy rainfall during the warm season in south china
publisher Wiley
series Atmospheric Science Letters
issn 1530-261X
publishDate 2020-06-01
description Abstract This article aims to examine the diurnal variation of heavy rainfall (HR) for various intensities and investigate duration and environment of HR during the warm season over South China. Results show that the HR mainly occurred in the late afternoon over most regions of Guangdong Province (GD) and east of Guangxi Province (GX), as well as the nocturnal‐to‐morning rainfall over the mountainous regions of northwestern GX and contiguous regions among GD. It exhibited two diurnal peaks in the early morning and in the late afternoon. HR which mostly occurred during the late afternoon by 1,700–1,900 LST exhibited longer durations (3–4 hr). The enhanced southerly wind and northerly wind over the mountainous, as well as the enhancement associated with strong horizontal surface‐temperature gradient due to surface heating and stronger vertical wind shear in the lower troposphere, contributed to the high‐frequency occurrences of the rainfall in the late afternoon.
topic atmosphere
geophysical sphere
observational data analysis
physical phenomenon
rainfall
seasonal scale
url https://doi.org/10.1002/asl.969
work_keys_str_mv AT shuixinzhong diurnalvariationofthedurationandenvironmentforheavyrainfallduringthewarmseasoninsouthchina
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