Runoff Coefficient in the Air Bengkulu Watershed and the Evaluation of the Existing Spatial Planning

Runoff coefficient plays a crucial role in estimating the peak discharge of a river basin. Therefore, this research aimed to investigate runoff coefficient in the Air Bengkulu watershed based on temporal land cover data and evaluate the existing spatial planning. Land cover data from 1998, 2002, 2016, and 2023, with spatial patterns derived from current regional planning were used. The temporal and spatial pattern-based runoff coefficients were determined using land cover data and spatial pattern function, respectively. Meanwhile, descriptive and comparative methods were adopted based on time. The calculated runoff coefficient was 0.073, 0.093, 0.276, and 0.273 for 1998, 2002, 2016, and 2023, while the value obtained based on spatial patterns was 0.306. Additionally, a general trend of increasing the values over time was observed. Land cover change, particularly the decline of forest areas and the expansion of settlement and plantation, contributed to the rising runoff coefficient. The results showed that runoff coefficient (0.306) exceeded the current land cover, similar to other analyses with higher runoff in the predicted scenario. This research suggested a need for a more detailed classification system and scale to accommodate land cover types with relatively low runoff coefficient. In risk assessment, land cover-like spatial patterns with low runoff coefficient should be placed as capacity other than vulnerability components.

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Publication Details

Journal
Indonesian Journal of Geography
Published
2024-08-14
DOI
https://doi.org/10.22146/ijg.91397
Primary Topic
Water and Land Management
Type
article
Field-Weighted Citation Impact
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article

Runoff Coefficient in the Air Bengkulu Watershed and the Evaluation of the Existing Spatial Planning

Teguh Adiprasetyo, Bambang Sulistyo, Noviyanti Listyaningrum, Bambang Gonggo Murcitro et al.
Indonesian Journal of Geography
Water and Land Management
article

Runoff Coefficient in the Air Bengkulu Watershed and the Evaluation of the Existing Spatial Planning

Teguh Adiprasetyo, Bambang Sulistyo, Noviyanti Listyaningrum, Bambang Gonggo Murcitro, Agus Joko Purwadi
article en

Abstract

Runoff coefficient plays a crucial role in estimating the peak discharge of a river basin. Therefore, this research aimed to investigate runoff coefficient in the Air Bengkulu watershed based on temporal land cover data and evaluate the existing spatial planning. Land cover data from 1998, 2002, 2016, and 2023, with spatial patterns derived from current regional planning were used. The temporal and spatial pattern-based runoff coefficients were determined using land cover data and spatial pattern function, respectively. Meanwhile, descriptive and comparative methods were adopted based on time. The calculated runoff coefficient was 0.073, 0.093, 0.276, and 0.273 for 1998, 2002, 2016, and 2023, while the value obtained based on spatial patterns was 0.306. Additionally, a general trend of increasing the values over time was observed. Land cover change, particularly the decline of forest areas and the expansion of settlement and plantation, contributed to the rising runoff coefficient. The results showed that runoff coefficient (0.306) exceeded the current land cover, similar to other analyses with higher runoff in the predicted scenario. This research suggested a need for a more detailed classification system and scale to accommodate land cover types with relatively low runoff coefficient. In risk assessment, land cover-like spatial patterns with low runoff coefficient should be placed as capacity other than vulnerability components.

Indonesian Journal of GeographyVol. 56(2)
Universitas Gadjah Mada (ID), University of Bengkulu (ID)
Universitas Bengkulu
Openalex Percentile: Top 77%
Water and Land Management
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Runoff Coefficient in the Air Bengkulu Watershed and the Evaluation of the Existing Spatial Planning — Teguh Adiprasetyo, Bambang Sulistyo, et al. · Indonesian Journal of Geography (2024) | TGRS Research Map | TGRS