HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia

The rapid development of Yogyakarta has made city development increase. This construction continues to expand the reach of impervious surfaces. As a result, surface runoff and maximum discharge have increased, overflowing up to urban drainage. This study aimed to analyze the maximum discharge of the...

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Main Authors: Slamet Suprayogi, Rifa'i, Reviana Latifah
Format: Article
Language:English
Published: Universitas Gadjah Mada 2021-04-01
Series:ASEAN Journal on Science and Technology for Development
Subjects:
Online Access:http://ajstd.org/index.php/ajstd/article/view/643
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spelling doaj-26d1c8bc81e04b59adfde3f5c3eaf46d2021-06-24T08:15:05ZengUniversitas Gadjah MadaASEAN Journal on Science and Technology for Development0217-54602224-90282021-04-0138115–2015–2010.29037/ajstd.643713HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, IndonesiaSlamet Suprayogi0Rifa'i1Reviana Latifah2Department of Environmental Geography, Faculty of Geography, Universitas Gadjah Mada, Sekip Utara, Bulaksumur, Yogyakarta 55281, IndonesiaDepartment of Environmental Geography, Faculty of Geography, Universitas Gadjah Mada, Sekip Utara, Bulaksumur, Yogyakarta 55281, IndonesiaDepartment of Environmental Geography, Faculty of Geography, Universitas Gadjah Mada, Sekip Utara, Bulaksumur, Yogyakarta 55281, IndonesiaThe rapid development of Yogyakarta has made city development increase. This construction continues to expand the reach of impervious surfaces. As a result, surface runoff and maximum discharge have increased, overflowing up to urban drainage. This study aimed to analyze the maximum discharge of the watershed based on design storms with 2, 5, 10, and 25-year return periods, used for flood control considerations. The urban flood was modelled using HEC-HMS. The results showed that the contribution of discharge flow in each segment is influenced by the dominance of land use, in which the segment dominated by dense settlements has a high contribution to the maximum discharge. The flow contribution is due to the high curve number value, which corresponds to the high surface runoff. The peak discharge of watersheds with return periods of 2, 5, 10, and 25 years are 8 m3/s, 20.1 m3/s, 29.9 m3/s, and 44.1 m3/s, respectively.http://ajstd.org/index.php/ajstd/article/view/643floodhec-hmsindonesiaurban
collection DOAJ
language English
format Article
sources DOAJ
author Slamet Suprayogi
Rifa'i
Reviana Latifah
spellingShingle Slamet Suprayogi
Rifa'i
Reviana Latifah
HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
ASEAN Journal on Science and Technology for Development
flood
hec-hms
indonesia
urban
author_facet Slamet Suprayogi
Rifa'i
Reviana Latifah
author_sort Slamet Suprayogi
title HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
title_short HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
title_full HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
title_fullStr HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
title_full_unstemmed HEC-HMS Model for Urban Flood Analysis in Belik River, Yogyakarta, Indonesia
title_sort hec-hms model for urban flood analysis in belik river, yogyakarta, indonesia
publisher Universitas Gadjah Mada
series ASEAN Journal on Science and Technology for Development
issn 0217-5460
2224-9028
publishDate 2021-04-01
description The rapid development of Yogyakarta has made city development increase. This construction continues to expand the reach of impervious surfaces. As a result, surface runoff and maximum discharge have increased, overflowing up to urban drainage. This study aimed to analyze the maximum discharge of the watershed based on design storms with 2, 5, 10, and 25-year return periods, used for flood control considerations. The urban flood was modelled using HEC-HMS. The results showed that the contribution of discharge flow in each segment is influenced by the dominance of land use, in which the segment dominated by dense settlements has a high contribution to the maximum discharge. The flow contribution is due to the high curve number value, which corresponds to the high surface runoff. The peak discharge of watersheds with return periods of 2, 5, 10, and 25 years are 8 m3/s, 20.1 m3/s, 29.9 m3/s, and 44.1 m3/s, respectively.
topic flood
hec-hms
indonesia
urban
url http://ajstd.org/index.php/ajstd/article/view/643
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AT revianalatifah hechmsmodelforurbanfloodanalysisinbelikriveryogyakartaindonesia
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