Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten

Based on data from the National Disaster Management Agency (Ind.: Badan Nasional Penanggulangan Bencana – BNPB), throughout 2022, more than 91% of disaster events were hydrometeorological disasters, with floods at 43% and landslides at 17%. One of the factors for floods and landslides is high rainfa...

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Published in:Journal of Water and Land Development
Main Authors: Hartanto, Syahrul Humaidi, Erna Frida, Naufal Ananda, Marzuki Sinambela
Format: Article
Language:English
Published: Polish Academy of Sciences 2024-10-01
Subjects:
Online Access:https://journals.pan.pl/Content/132983/2024-03-JWLD-22.pdf
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author Hartanto
Syahrul Humaidi
Erna Frida
Naufal Ananda
Marzuki Sinambela
author_facet Hartanto
Syahrul Humaidi
Erna Frida
Naufal Ananda
Marzuki Sinambela
author_sort Hartanto
collection DOAJ
container_title Journal of Water and Land Development
description Based on data from the National Disaster Management Agency (Ind.: Badan Nasional Penanggulangan Bencana – BNPB), throughout 2022, more than 91% of disaster events were hydrometeorological disasters, with floods at 43% and landslides at 17%. One of the factors for floods and landslides is high rainfall intensity. Automatic rain gauge (ARG) is a rainfall observation instrument that can accurately measure rainfall at observation points. However, it has problems such as communication systems that cause delays in data transmission, low instrument density, and inability to cover a wide spatial area, which can affect the accuracy of rainfall information. Weather radar is a remote sensing instrument that can estimate rainfall spatially so that weather radar observations can reach areas of the region that do not have ARG. However, before being used as rainfall information, estimation rainfall needs to be evaluated or calibrated. Evaluation of rainfall estimation on weather radar to ARG in Banten at a 30– 120 km distance range, shows a coefficient of determination above 0.8. Based on the studies that have been conducted, increase of root mean square error (RMSE) is due to influence of radar observation range and observation distance on ARG. Adjustment of rainfall estimation improves the accuracy of rainfall estimation. Adjusting rainfall estimation can reduce RMSE by 50%.
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spelling doaj-art-3c9eb79f2ee042bcbc3f4c2e8d80547b2025-08-20T01:45:06ZengPolish Academy of SciencesJournal of Water and Land Development2083-45352024-10-01No 62193200https://doi.org/10.24425/jwld.2024.151567Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in BantenHartanto0https://orcid.org/0009-0008-9287-072XSyahrul Humaidi1https://orcid.org/0000-0003-2183-3282Erna Frida2https://orcid.org/0000-0001-8953-9499Naufal Ananda3https://orcid.org/0009-0009-9965-4402Marzuki Sinambela4https://orcid.org/0000-0003-3363-4440Universitas Sumatera Utara, FMIPA, Post Graduate Program (Physics), Bioteknologi St No. 1, USU, 20155, Medan, IndonesiaUniversitas Sumatera Utara, FMIPA, Post Graduate Program (Physics), Bioteknologi St No. 1, USU, 20155, Medan, IndonesiaUniversitas Sumatera Utara, FMIPA, Post Graduate Program (Physics), Bioteknologi St No. 1, USU, 20155, Medan, IndonesiaInstitut Teknologi Bandung, Graduate Student in Instrumentation & Control Program, Ganesha St No. 1, 40132, Bandung, IndonesiaSekolah Tinggi Meteorologi Klimatologi dan Geofisika, Program in Applied of Instrumentation, MKG, Meteorologi No. 5 Tanah Tinggi, 15119, Tangerang, Banten, Jakarta, IndonesiaBased on data from the National Disaster Management Agency (Ind.: Badan Nasional Penanggulangan Bencana – BNPB), throughout 2022, more than 91% of disaster events were hydrometeorological disasters, with floods at 43% and landslides at 17%. One of the factors for floods and landslides is high rainfall intensity. Automatic rain gauge (ARG) is a rainfall observation instrument that can accurately measure rainfall at observation points. However, it has problems such as communication systems that cause delays in data transmission, low instrument density, and inability to cover a wide spatial area, which can affect the accuracy of rainfall information. Weather radar is a remote sensing instrument that can estimate rainfall spatially so that weather radar observations can reach areas of the region that do not have ARG. However, before being used as rainfall information, estimation rainfall needs to be evaluated or calibrated. Evaluation of rainfall estimation on weather radar to ARG in Banten at a 30– 120 km distance range, shows a coefficient of determination above 0.8. Based on the studies that have been conducted, increase of root mean square error (RMSE) is due to influence of radar observation range and observation distance on ARG. Adjustment of rainfall estimation improves the accuracy of rainfall estimation. Adjusting rainfall estimation can reduce RMSE by 50%.https://journals.pan.pl/Content/132983/2024-03-JWLD-22.pdfestimationmarshall–palmerrainfallreflectivityweather radar
spellingShingle Hartanto
Syahrul Humaidi
Erna Frida
Naufal Ananda
Marzuki Sinambela
Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
estimation
marshall–palmer
rainfall
reflectivity
weather radar
title Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
title_full Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
title_fullStr Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
title_full_unstemmed Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
title_short Spatial evaluation rainfall estimation on weather radar using Marshall–Palmer reflectivity–rainfall rate in Banten
title_sort spatial evaluation rainfall estimation on weather radar using marshall palmer reflectivity rainfall rate in banten
topic estimation
marshall–palmer
rainfall
reflectivity
weather radar
url https://journals.pan.pl/Content/132983/2024-03-JWLD-22.pdf
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AT ernafrida spatialevaluationrainfallestimationonweatherradarusingmarshallpalmerreflectivityrainfallrateinbanten
AT naufalananda spatialevaluationrainfallestimationonweatherradarusingmarshallpalmerreflectivityrainfallrateinbanten
AT marzukisinambela spatialevaluationrainfallestimationonweatherradarusingmarshallpalmerreflectivityrainfallrateinbanten