Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China

An extremely heavy rainfall event hit Guangdong province, China, from 27 August to 1 September 2018. There were two different extreme rain regions, respectively, at the Pearl River estuary and eastern Guangdong, and a record-breaking daily precipitation of 1056.7 mm was observed at Gaotan station on...

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Main Authors: Yu Ma, Haonan Chen, Guangheng Ni, V. Chandrasekar, Yabin Gou, Wenjuan Zhang
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/17/2772
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author Yu Ma
Haonan Chen
Guangheng Ni
V. Chandrasekar
Yabin Gou
Wenjuan Zhang
author_facet Yu Ma
Haonan Chen
Guangheng Ni
V. Chandrasekar
Yabin Gou
Wenjuan Zhang
author_sort Yu Ma
collection DOAJ
description An extremely heavy rainfall event hit Guangdong province, China, from 27 August to 1 September 2018. There were two different extreme rain regions, respectively, at the Pearl River estuary and eastern Guangdong, and a record-breaking daily precipitation of 1056.7 mm was observed at Gaotan station on 30 August. This paper utilizes a suite of observations from soundings, a gauge network, disdrometers, and polarimetric radars to gain insights to the two rainfall centers. The large-scale meteorological forcing, rainfall patterns, and microphysical processes, as well as radar-based precipitation signatures are investigated. It is concluded that a west-moving monsoon depression played a critical role in sustaining the moisture supply to the two extreme rain regions, and the combined orographic enhancement further contributed to the torrential rainfall over Gaotan station. The raindrop size distributions (DSD) observed at Zhuhai and Huidong stations, as well as the observed polarimetric radar signatures indicate that the rainfall at Doumen region was characterized by larger raindrops but a lower number concentration compared with that at Gaotan region. In addition, the dual-polarization radars are used to quantify precipitation intensity during this extreme event, providing timely information for flood warning and emergency management decision-making.
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spelling doaj.art-61af938cb17248d6b9ee900ffd92646f2023-11-20T11:26:40ZengMDPI AGRemote Sensing2072-42922020-08-011217277210.3390/rs12172772Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern ChinaYu Ma0Haonan Chen1Guangheng Ni2V. Chandrasekar3Yabin Gou4Wenjuan Zhang5Department of Hydraulic Engineering, State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, ChinaElectrical and Computer Engineering, Colorado State University, Fort Collins, CO 80523, USADepartment of Hydraulic Engineering, State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, ChinaElectrical and Computer Engineering, Colorado State University, Fort Collins, CO 80523, USAHangzhou Meteorological Bureau, Hangzhou 310051, ChinaState Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, ChinaAn extremely heavy rainfall event hit Guangdong province, China, from 27 August to 1 September 2018. There were two different extreme rain regions, respectively, at the Pearl River estuary and eastern Guangdong, and a record-breaking daily precipitation of 1056.7 mm was observed at Gaotan station on 30 August. This paper utilizes a suite of observations from soundings, a gauge network, disdrometers, and polarimetric radars to gain insights to the two rainfall centers. The large-scale meteorological forcing, rainfall patterns, and microphysical processes, as well as radar-based precipitation signatures are investigated. It is concluded that a west-moving monsoon depression played a critical role in sustaining the moisture supply to the two extreme rain regions, and the combined orographic enhancement further contributed to the torrential rainfall over Gaotan station. The raindrop size distributions (DSD) observed at Zhuhai and Huidong stations, as well as the observed polarimetric radar signatures indicate that the rainfall at Doumen region was characterized by larger raindrops but a lower number concentration compared with that at Gaotan region. In addition, the dual-polarization radars are used to quantify precipitation intensity during this extreme event, providing timely information for flood warning and emergency management decision-making.https://www.mdpi.com/2072-4292/12/17/2772extreme rainfallpolarimetric radar signaturesquantitative precipitation estimationsouthern china
spellingShingle Yu Ma
Haonan Chen
Guangheng Ni
V. Chandrasekar
Yabin Gou
Wenjuan Zhang
Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
Remote Sensing
extreme rainfall
polarimetric radar signatures
quantitative precipitation estimation
southern china
title Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
title_full Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
title_fullStr Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
title_full_unstemmed Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
title_short Microphysical and Polarimetric Radar Signatures of an Epic Flood Event in Southern China
title_sort microphysical and polarimetric radar signatures of an epic flood event in southern china
topic extreme rainfall
polarimetric radar signatures
quantitative precipitation estimation
southern china
url https://www.mdpi.com/2072-4292/12/17/2772
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