Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area

For disaster monitoring and mitigation, an X-Band polarimetric radar can provide one or two minutes of rainfall data in small areas. However, this weather radar is not available in tropical nations such as Malaysia, which has suffered from flash floods and flooding, particularly during the monsoon s...

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Published in:Science and Technology Asia
Main Author: Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
Format: Article
Language:English
Published: Thammasat University 2024
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85206574493&partnerID=40&md5=a1ca117d576f8a80dde433cb88089704
id 2-s2.0-85206574493
spelling 2-s2.0-85206574493
Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
2024
Science and Technology Asia
29
3

https://www.scopus.com/inward/record.uri?eid=2-s2.0-85206574493&partnerID=40&md5=a1ca117d576f8a80dde433cb88089704
For disaster monitoring and mitigation, an X-Band polarimetric radar can provide one or two minutes of rainfall data in small areas. However, this weather radar is not available in tropical nations such as Malaysia, which has suffered from flash floods and flooding, particularly during the monsoon season. As a result, this study evaluates rainfall estimation strategies for small drainage regions as part of a proposal for a new framework of rainfall estimation in Malaysia that employs X-Band polarimetric radar. It begins with raw data conversion, then clips the DEM, selects the drainage area in Kagoshima, and finally plots the hyetograph for rainfall events. The extraction of X-Band polarimetric rainfall data from AMeDAS ground data was investigated. The statistical validation results reveal a relatively positive association between X-Band polarimetry and AMeDAS, with an R2 value of around 24% for model fit. Furthermore, using QGIS to compare rainfall distribution results for both data sets reveals that AMeDAS data does not accurately reflect actual rainfall monitored by X-Band polarimetric radar because there are no AMeDAS stations in the drainage area, and the X-Band polarimetric radar distribution image is also real-time. All drainages were classified as heavy rain in the upper stream, indicating the precise location of the highest intensity and the possibility that the area closest to the drainage would experience a disaster such as a flood. This paper concludes with suggestions for future works. © 2024, Thammasat University. All rights reserved.
Thammasat University
25869027
English
Article

author Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
spellingShingle Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
author_facet Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
author_sort Hasan N.A.; Goto M.; Miyamoto K.; Iguchi M.; Tamunaidu P.; Ros F.C.
title Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
title_short Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
title_full Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
title_fullStr Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
title_full_unstemmed Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
title_sort Rainfall Data Assessment from X-Band Polarimetric Radar for Small Drainage Area
publishDate 2024
container_title Science and Technology Asia
container_volume 29
container_issue 3
doi_str_mv
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85206574493&partnerID=40&md5=a1ca117d576f8a80dde433cb88089704
description For disaster monitoring and mitigation, an X-Band polarimetric radar can provide one or two minutes of rainfall data in small areas. However, this weather radar is not available in tropical nations such as Malaysia, which has suffered from flash floods and flooding, particularly during the monsoon season. As a result, this study evaluates rainfall estimation strategies for small drainage regions as part of a proposal for a new framework of rainfall estimation in Malaysia that employs X-Band polarimetric radar. It begins with raw data conversion, then clips the DEM, selects the drainage area in Kagoshima, and finally plots the hyetograph for rainfall events. The extraction of X-Band polarimetric rainfall data from AMeDAS ground data was investigated. The statistical validation results reveal a relatively positive association between X-Band polarimetry and AMeDAS, with an R2 value of around 24% for model fit. Furthermore, using QGIS to compare rainfall distribution results for both data sets reveals that AMeDAS data does not accurately reflect actual rainfall monitored by X-Band polarimetric radar because there are no AMeDAS stations in the drainage area, and the X-Band polarimetric radar distribution image is also real-time. All drainages were classified as heavy rain in the upper stream, indicating the precise location of the highest intensity and the possibility that the area closest to the drainage would experience a disaster such as a flood. This paper concludes with suggestions for future works. © 2024, Thammasat University. All rights reserved.
publisher Thammasat University
issn 25869027
language English
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