Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season

A torrential rain episode (≥ 200 mm day-1) was observed over coastal regions of southern Taiwan (south of 23.0°N) on 5 June 2008 under the influence of a meso-scale frontal cyclone (MFC) formed along the western flank of a Mei-yu frontal zone. Through the incorporation of additional observations ove...

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Main Author: Hsi-Chyi Yeh Shui-Shang Chi
Format: Article
Language:English
Published: Chinese Geoscience Union 2013-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v241p069.pdf
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spelling doaj-a89ab73a305449caa72f75ac2f025ffc2020-11-25T00:25:40ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802013-01-0124106910.3319/TAO.2012.09.03.01(A)1112Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu SeasonHsi-Chyi Yeh Shui-Shang ChiA torrential rain episode (≥ 200 mm day-1) was observed over coastal regions of southern Taiwan (south of 23.0°N) on 5 June 2008 under the influence of a meso-scale frontal cyclone (MFC) formed along the western flank of a Mei-yu frontal zone. Through the incorporation of additional observations over the ocean collected during Southwest Monsoon Experiment (SoWMEX)/Terrain-influenced Monsoon Rainfall Experiment (TiMREX), the location of a Mei-yu frontal boundary, defined by the wind shift, is better identified over the open ocean by the data assimilation of dropsonde observations. Meanwhile, the low-level cyclonic vorticity and horizontal convergence are increased along the Mei-yu frontal zone, and an increment maximum center of cyclonic vorticity locates over the north of South China Sea (SCS), where the MFC subsequently forms. http://tao.cgu.org.tw/images/attachments/v241p069.pdf Torrential rainMei-yuSoWMEX/TiMREXData assimilation
collection DOAJ
language English
format Article
sources DOAJ
author Hsi-Chyi Yeh Shui-Shang Chi
spellingShingle Hsi-Chyi Yeh Shui-Shang Chi
Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
Terrestrial, Atmospheric and Oceanic Sciences
Torrential rain
Mei-yu
SoWMEX/TiMREX
Data assimilation
author_facet Hsi-Chyi Yeh Shui-Shang Chi
author_sort Hsi-Chyi Yeh Shui-Shang Chi
title Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
title_short Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
title_full Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
title_fullStr Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
title_full_unstemmed Prediction of a Mei-yu Frontal Cyclone and the Associated Torrential Rainfall over Southern Taiwan During 2008 Mei-yu Season
title_sort prediction of a mei-yu frontal cyclone and the associated torrential rainfall over southern taiwan during 2008 mei-yu season
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2013-01-01
description A torrential rain episode (≥ 200 mm day-1) was observed over coastal regions of southern Taiwan (south of 23.0°N) on 5 June 2008 under the influence of a meso-scale frontal cyclone (MFC) formed along the western flank of a Mei-yu frontal zone. Through the incorporation of additional observations over the ocean collected during Southwest Monsoon Experiment (SoWMEX)/Terrain-influenced Monsoon Rainfall Experiment (TiMREX), the location of a Mei-yu frontal boundary, defined by the wind shift, is better identified over the open ocean by the data assimilation of dropsonde observations. Meanwhile, the low-level cyclonic vorticity and horizontal convergence are increased along the Mei-yu frontal zone, and an increment maximum center of cyclonic vorticity locates over the north of South China Sea (SCS), where the MFC subsequently forms.
topic Torrential rain
Mei-yu
SoWMEX/TiMREX
Data assimilation
url http://tao.cgu.org.tw/images/attachments/v241p069.pdf
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