Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability

The characteristics of nocturnal-to-morning rainfall (NMR) during the warm season in South China are examined using hourly surface observations from 2015–2019. Results show that strong NMR is mainly located in coastal regions and mountainous areas. NMR mainly occurs during 0200–0800 LST. The distrib...

Full description

Bibliographic Details
Main Authors: Shuixin ZHONG, Shuai YANG
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2020-11-01
Series:Atmospheric and Oceanic Science Letters
Subjects:
Online Access:http://dx.doi.org/10.1080/16742834.2020.1820844
id doaj-638c040f19364217b73fb1af0f7152fa
record_format Article
spelling doaj-638c040f19364217b73fb1af0f7152fa2021-04-02T19:05:56ZengKeAi Communications Co., Ltd.Atmospheric and Oceanic Science Letters1674-28342376-61232020-11-0113652753310.1080/16742834.2020.18208441820844Nocturnal-to-morning rains during the warm season in South China: characteristics and predictabilityShuixin ZHONG0Shuai YANG1Institute of Tropical and Marine Meteorology, CMAInstitute of Atmospheric Physics Chinese Academy of SciencesThe characteristics of nocturnal-to-morning rainfall (NMR) during the warm season in South China are examined using hourly surface observations from 2015–2019. Results show that strong NMR is mainly located in coastal regions and mountainous areas. NMR mainly occurs during 0200–0800 LST. The distribution of NMR can be divided into two types. The first pattern is a coastal type where NMR is mainly located at windward sites, such as southern coastal mountain areas in Guangdong (GD) and in Guangxi (GX). The second type is an inland type where NMR is mainly located at windward sites, such as the northern mountainous areas in GX and the Pearl River Delta regions in GD. The strong convergence between the northerly wind over the mountainous regions and southerly wind, as well as the strong downhill winds strengthened by the narrow pipe effect over the valleys in mountainous areas, together contribute to the high frequency of inland NMR. The strong southeasterly onshore wind and the cyclonic circulations strengthened by the northeasterly wind over the northern mountainous areas contribute to the high frequency of coastal NMR. Though the GRAPES (Global/Regional Assimilation and Prediction System) model can capture the intensity and distribution of large-scale NMR, it exhibits low predictability of small-scale NMR, especially that in the warm sector.http://dx.doi.org/10.1080/16742834.2020.1820844south chinawarm seasonnocturnal-to-morning rainfallgrapes
collection DOAJ
language English
format Article
sources DOAJ
author Shuixin ZHONG
Shuai YANG
spellingShingle Shuixin ZHONG
Shuai YANG
Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
Atmospheric and Oceanic Science Letters
south china
warm season
nocturnal-to-morning rainfall
grapes
author_facet Shuixin ZHONG
Shuai YANG
author_sort Shuixin ZHONG
title Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
title_short Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
title_full Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
title_fullStr Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
title_full_unstemmed Nocturnal-to-morning rains during the warm season in South China: characteristics and predictability
title_sort nocturnal-to-morning rains during the warm season in south china: characteristics and predictability
publisher KeAi Communications Co., Ltd.
series Atmospheric and Oceanic Science Letters
issn 1674-2834
2376-6123
publishDate 2020-11-01
description The characteristics of nocturnal-to-morning rainfall (NMR) during the warm season in South China are examined using hourly surface observations from 2015–2019. Results show that strong NMR is mainly located in coastal regions and mountainous areas. NMR mainly occurs during 0200–0800 LST. The distribution of NMR can be divided into two types. The first pattern is a coastal type where NMR is mainly located at windward sites, such as southern coastal mountain areas in Guangdong (GD) and in Guangxi (GX). The second type is an inland type where NMR is mainly located at windward sites, such as the northern mountainous areas in GX and the Pearl River Delta regions in GD. The strong convergence between the northerly wind over the mountainous regions and southerly wind, as well as the strong downhill winds strengthened by the narrow pipe effect over the valleys in mountainous areas, together contribute to the high frequency of inland NMR. The strong southeasterly onshore wind and the cyclonic circulations strengthened by the northeasterly wind over the northern mountainous areas contribute to the high frequency of coastal NMR. Though the GRAPES (Global/Regional Assimilation and Prediction System) model can capture the intensity and distribution of large-scale NMR, it exhibits low predictability of small-scale NMR, especially that in the warm sector.
topic south china
warm season
nocturnal-to-morning rainfall
grapes
url http://dx.doi.org/10.1080/16742834.2020.1820844
work_keys_str_mv AT shuixinzhong nocturnaltomorningrainsduringthewarmseasoninsouthchinacharacteristicsandpredictability
AT shuaiyang nocturnaltomorningrainsduringthewarmseasoninsouthchinacharacteristicsandpredictability
_version_ 1721549596276031488