Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java

Upper Citarik River is the Inter Mountainous Valley of Volcanic Denudational Landform in the eastern part of Bandung basin, West-Java. The research area compounds of several degraded small catchments with very low water flow in dry season. This research aims  to understand the implications of morpho...

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Main Authors: Edi Tri Haryanto, Emi Sukiyah, Pradnya Paramarta Raditya Rendra, Hendarmawan Hendarmawan, Suratman Suratman
Format: Article
Language:English
Published: Universitas Gadjah Mada 2019-08-01
Series:Indonesian Journal of Geography
Subjects:
Online Access:https://jurnal.ugm.ac.id/ijg/article/view/36472
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spelling doaj-82e15b81d68f44fe864e2a34487826612020-11-25T02:47:42ZengUniversitas Gadjah MadaIndonesian Journal of Geography0024-95212354-91142019-08-0151222423010.22146/ijg.3647224968Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West JavaEdi Tri Haryanto0Emi Sukiyah1Pradnya Paramarta Raditya Rendra2Hendarmawan Hendarmawan3Suratman Suratman4Padjadjaran University, Bandung, IndonesiaPadjadjaran University, Bandung, IndonesiaPadjadjaran University, Bandung, IndonesiaPadjadjaran University, Bandung, IndonesiaFaculty of Geography, Universitas Gadjah Mada, YogyakartaUpper Citarik River is the Inter Mountainous Valley of Volcanic Denudational Landform in the eastern part of Bandung basin, West-Java. The research area compounds of several degraded small catchments with very low water flow in dry season. This research aims  to understand the implications of morphometric characteristics (Slope, Cr, Dd, Hi) on average river flow discharge of small sub-catchments of Upper Citarik River. Discharge data collected based on measurements, while catchments morphometric identified and analyzed based on topographic map using GIS techniques.  Correlation graphs were used to understand the relationship among the morphometric parameter and the average river flow discharges. The result were as follow  the steeper the slope, the more elongated the shape of catchment, the more distant was the river density,  meaning the more younger the erosion cycle of the landform.  The younger the erosion cycle of the landform, the smaller was the average river discharge per areal unit of catchments.https://jurnal.ugm.ac.id/ijg/article/view/36472morphometry, river discharge, catchment, volcanic landform, bandung
collection DOAJ
language English
format Article
sources DOAJ
author Edi Tri Haryanto
Emi Sukiyah
Pradnya Paramarta Raditya Rendra
Hendarmawan Hendarmawan
Suratman Suratman
spellingShingle Edi Tri Haryanto
Emi Sukiyah
Pradnya Paramarta Raditya Rendra
Hendarmawan Hendarmawan
Suratman Suratman
Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
Indonesian Journal of Geography
morphometry, river discharge, catchment, volcanic landform, bandung
author_facet Edi Tri Haryanto
Emi Sukiyah
Pradnya Paramarta Raditya Rendra
Hendarmawan Hendarmawan
Suratman Suratman
author_sort Edi Tri Haryanto
title Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
title_short Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
title_full Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
title_fullStr Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
title_full_unstemmed Implication of Catchment Morphometric on Small River Discharge of Upper Citarik River, West Java
title_sort implication of catchment morphometric on small river discharge of upper citarik river, west java
publisher Universitas Gadjah Mada
series Indonesian Journal of Geography
issn 0024-9521
2354-9114
publishDate 2019-08-01
description Upper Citarik River is the Inter Mountainous Valley of Volcanic Denudational Landform in the eastern part of Bandung basin, West-Java. The research area compounds of several degraded small catchments with very low water flow in dry season. This research aims  to understand the implications of morphometric characteristics (Slope, Cr, Dd, Hi) on average river flow discharge of small sub-catchments of Upper Citarik River. Discharge data collected based on measurements, while catchments morphometric identified and analyzed based on topographic map using GIS techniques.  Correlation graphs were used to understand the relationship among the morphometric parameter and the average river flow discharges. The result were as follow  the steeper the slope, the more elongated the shape of catchment, the more distant was the river density,  meaning the more younger the erosion cycle of the landform.  The younger the erosion cycle of the landform, the smaller was the average river discharge per areal unit of catchments.
topic morphometry, river discharge, catchment, volcanic landform, bandung
url https://jurnal.ugm.ac.id/ijg/article/view/36472
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AT emisukiyah implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava
AT pradnyaparamartaradityarendra implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava
AT hendarmawanhendarmawan implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava
AT suratmansuratman implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava
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