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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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 |
work_keys_str_mv |
AT editriharyanto implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava AT emisukiyah implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava AT pradnyaparamartaradityarendra implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava AT hendarmawanhendarmawan implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava AT suratmansuratman implicationofcatchmentmorphometriconsmallriverdischargeofuppercitarikriverwestjava |
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1724751963080359936 |