Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1

Cempaka Tropical Cyclone (TC) occurred on November 27, 2017, at the Indian Ocean and induced high rainfall leading to flooding in the southern part of Java island. One of the most affected areas is the karst landscape of Gunung Sewu. This study aims to identify flood inundated areas caused by the Ce...

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Main Authors: Pambudi Ridwan Arif, Riadini Fitri, Naldi Ari, Putri Nadya Paramitha
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/62/e3sconf_icenis2020_03030.pdf
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spelling doaj-e468e5cf4488455a8ad3bd52936eb36f2021-04-02T17:10:25ZengEDP SciencesE3S Web of Conferences2267-12422020-01-012020303010.1051/e3sconf/202020203030e3sconf_icenis2020_03030Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1Pambudi Ridwan ArifRiadini Fitri0Naldi Ari1Putri Nadya ParamithaDepartment of Geography, Faculty of Mathematics and Natural Science, Universitas IndonesiaSchool of Environmental Science, Universitas IndonesiaCempaka Tropical Cyclone (TC) occurred on November 27, 2017, at the Indian Ocean and induced high rainfall leading to flooding in the southern part of Java island. One of the most affected areas is the karst landscape of Gunung Sewu. This study aims to identify flood inundated areas caused by the Cempaka TC in the Gunung Sewu karst landscape through satellite imagery of Sentinel 1B. Sentinel 1B imageries were used to extract the flood inundation area through the processing of random forest (RF) and the thresholding value (TV). A significant difference in flood inundated area was obtained between RF and TV, where RF shows a result of 526.07 ha of the total inundated area while the TV shows a result of 105.46 ha. However, both methods show the same sequence for three regencies with the highest total flood inundated area (Gunungkidul, Pacitan, and Wonogiri) and show the same range of each flood inundated area (0-0.5 ha). This distribution of flood inundated area can be used by policymakers as a basis for spatial planning in Gunung Sewu karst landscape.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/62/e3sconf_icenis2020_03030.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Pambudi Ridwan Arif
Riadini Fitri
Naldi Ari
Putri Nadya Paramitha
spellingShingle Pambudi Ridwan Arif
Riadini Fitri
Naldi Ari
Putri Nadya Paramitha
Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
E3S Web of Conferences
author_facet Pambudi Ridwan Arif
Riadini Fitri
Naldi Ari
Putri Nadya Paramitha
author_sort Pambudi Ridwan Arif
title Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
title_short Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
title_full Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
title_fullStr Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
title_full_unstemmed Flood Inundation Mapping of Cempaka Tropical Cyclone Effect in Gunung Sewu Karst Landscape Using Sentinel 1
title_sort flood inundation mapping of cempaka tropical cyclone effect in gunung sewu karst landscape using sentinel 1
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Cempaka Tropical Cyclone (TC) occurred on November 27, 2017, at the Indian Ocean and induced high rainfall leading to flooding in the southern part of Java island. One of the most affected areas is the karst landscape of Gunung Sewu. This study aims to identify flood inundated areas caused by the Cempaka TC in the Gunung Sewu karst landscape through satellite imagery of Sentinel 1B. Sentinel 1B imageries were used to extract the flood inundation area through the processing of random forest (RF) and the thresholding value (TV). A significant difference in flood inundated area was obtained between RF and TV, where RF shows a result of 526.07 ha of the total inundated area while the TV shows a result of 105.46 ha. However, both methods show the same sequence for three regencies with the highest total flood inundated area (Gunungkidul, Pacitan, and Wonogiri) and show the same range of each flood inundated area (0-0.5 ha). This distribution of flood inundated area can be used by policymakers as a basis for spatial planning in Gunung Sewu karst landscape.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/62/e3sconf_icenis2020_03030.pdf
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