Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia

River flood has become a severe disruption toward the community, and it can trigger loss of life, damage infrastructure and properties, suffer economic, social and cultural, and environmental degradation. Flood hazard analysis downstream of Comal Watershed in Pemalang Regency, Central Java, was desi...

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Main Authors: Wibowo, Y. A., Marfai, M. A., Hadi, M. P., Fatchurohman, H., Ronggowulan, L., Arif, D. A.
Format: Conference or Workshop Item PeerReviewed
Language:English
Published: 2022
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Online Access:https://repository.ugm.ac.id/280277/1/Geospatial%20technology%20for%20flood%20hazard%20analysis%20in%20Comal%20Watershed%2C%20Central%20Java%2C%20Indonesia.pdf
https://repository.ugm.ac.id/280277/
https://iopscience.iop.org/article/10.1088/1755-1315/1039/1/012027
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Institution: Universitas Gadjah Mada
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spelling id-ugm-repo.2802772023-11-08T06:36:19Z https://repository.ugm.ac.id/280277/ Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia Wibowo, Y. A. Marfai, M. A. Hadi, M. P. Fatchurohman, H. Ronggowulan, L. Arif, D. A. Geography and Environmental Sciences River flood has become a severe disruption toward the community, and it can trigger loss of life, damage infrastructure and properties, suffer economic, social and cultural, and environmental degradation. Flood hazard analysis downstream of Comal Watershed in Pemalang Regency, Central Java, was designed to generate the flood hazard map to reduce the effects of flood disaster. The flood hazard was simulated for five, 10, 25, and 50 years using HEC-RAS and ArcGIS with HEC-GeoRAS. The data input was discharge, geometry, and roughness. The discharge was obtained from hydrology modelling by utilizing daily rainfall data for 22 years. The geometry data was composed of a topographic map and measured using an echo sounder, while the roughness was from land use along the flood plain. The accuracy and validation were conducted by matching the flood modelling result with the historical data from the Pemalang Disaster Management Agency and in-depth interview results with the community. The results showed the Comal River downstream flood hazard was feasible for disaster risk reduction purposes. The flood hazard levels were generated in five, 10, 25, and 50 years return periods dominated by high and very low levels. In every return period, the rising trend of the inundation width and the flood depth occurred for very high, high, and very low levels. 2022 Conference or Workshop Item PeerReviewed application/pdf en https://repository.ugm.ac.id/280277/1/Geospatial%20technology%20for%20flood%20hazard%20analysis%20in%20Comal%20Watershed%2C%20Central%20Java%2C%20Indonesia.pdf Wibowo, Y. A. and Marfai, M. A. and Hadi, M. P. and Fatchurohman, H. and Ronggowulan, L. and Arif, D. A. (2022) Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia. In: 4th International Conference on Environmental Resources Management (ICERM-2021), 1 November 2021, Virtual. https://iopscience.iop.org/article/10.1088/1755-1315/1039/1/012027
institution Universitas Gadjah Mada
building UGM Library
continent Asia
country Indonesia
Indonesia
content_provider UGM Library
collection Repository Civitas UGM
language English
topic Geography and Environmental Sciences
spellingShingle Geography and Environmental Sciences
Wibowo, Y. A.
Marfai, M. A.
Hadi, M. P.
Fatchurohman, H.
Ronggowulan, L.
Arif, D. A.
Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
description River flood has become a severe disruption toward the community, and it can trigger loss of life, damage infrastructure and properties, suffer economic, social and cultural, and environmental degradation. Flood hazard analysis downstream of Comal Watershed in Pemalang Regency, Central Java, was designed to generate the flood hazard map to reduce the effects of flood disaster. The flood hazard was simulated for five, 10, 25, and 50 years using HEC-RAS and ArcGIS with HEC-GeoRAS. The data input was discharge, geometry, and roughness. The discharge was obtained from hydrology modelling by utilizing daily rainfall data for 22 years. The geometry data was composed of a topographic map and measured using an echo sounder, while the roughness was from land use along the flood plain. The accuracy and validation were conducted by matching the flood modelling result with the historical data from the Pemalang Disaster Management Agency and in-depth interview results with the community. The results showed the Comal River downstream flood hazard was feasible for disaster risk reduction purposes. The flood hazard levels were generated in five, 10, 25, and 50 years return periods dominated by high and very low levels. In every return period, the rising trend of the inundation width and the flood depth occurred for very high, high, and very low levels.
format Conference or Workshop Item
PeerReviewed
author Wibowo, Y. A.
Marfai, M. A.
Hadi, M. P.
Fatchurohman, H.
Ronggowulan, L.
Arif, D. A.
author_facet Wibowo, Y. A.
Marfai, M. A.
Hadi, M. P.
Fatchurohman, H.
Ronggowulan, L.
Arif, D. A.
author_sort Wibowo, Y. A.
title Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
title_short Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
title_full Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
title_fullStr Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
title_full_unstemmed Geospatial technology for flood hazard analysis in Comal Watershed, Central Java, Indonesia
title_sort geospatial technology for flood hazard analysis in comal watershed, central java, indonesia
publishDate 2022
url https://repository.ugm.ac.id/280277/1/Geospatial%20technology%20for%20flood%20hazard%20analysis%20in%20Comal%20Watershed%2C%20Central%20Java%2C%20Indonesia.pdf
https://repository.ugm.ac.id/280277/
https://iopscience.iop.org/article/10.1088/1755-1315/1039/1/012027
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