Prediction of Runoff in Watersheds Located within Data-Scarce Regions

The interest in the use of mathematical models for the simulation of hydrological processes has largely increased especially in the prediction of runoff. It is the subject of extreme research among engineers and hydrologists. This study attempts to develop a simple conceptual model that reflects the...

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Main Authors: Ghanim, A.A.J., Beddu, S., Abd Manan, T.S.B., Al Yami, S.H., Irfan, M., Mursal, S.N.F., Mohd Kamal, N.L., Mohamad, D., Machmudah, A., Yavari, S., Mohtar, W.H.M.W., Ahmad, A., Rasdi, N.W., Khan, T.
Format: Article
Published: MDPI 2022
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85133551325&doi=10.3390%2fsu14137986&partnerID=40&md5=610f27998c860a98fda1ee8d2d41a422
http://eprints.utp.edu.my/33363/
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spelling my.utp.eprints.333632022-07-26T08:19:57Z Prediction of Runoff in Watersheds Located within Data-Scarce Regions Ghanim, A.A.J. Beddu, S. Abd Manan, T.S.B. Al Yami, S.H. Irfan, M. Mursal, S.N.F. Mohd Kamal, N.L. Mohamad, D. Machmudah, A. Yavari, S. Mohtar, W.H.M.W. Ahmad, A. Rasdi, N.W. Khan, T. The interest in the use of mathematical models for the simulation of hydrological processes has largely increased especially in the prediction of runoff. It is the subject of extreme research among engineers and hydrologists. This study attempts to develop a simple conceptual model that reflects the features of the arid environment where the availability of hydrological data is scarce. The model simulates an hourly streamflow hydrograph and the peak flow rate for any given storm. Hourly rainfall, potential evapotranspiration, and streamflow record are the significant input prerequisites for this model. The proposed model applied two (2) different hydrologic routing techniques: the time area curve method (wetted area of the catchment) and the Muskingum method (catchment main channel). The model was calibrated and analyzed based on the data collected from arid catchment in the center of Jordan. The model performance was evaluated via goodness of fit. The simulation of the proposed model fits both (a) observed and simulated streamflow and (b) observed and simulated peak flow rate. The model has the potential to be used for peak discharges� prediction during a storm period. The modeling approach described in this study has to be tested in additional catchments with appropriate data length in order to attain reliable model parameters. © 2022 by the authors. Licensee MDPI, Basel, Switzerland. MDPI 2022 Article NonPeerReviewed https://www.scopus.com/inward/record.uri?eid=2-s2.0-85133551325&doi=10.3390%2fsu14137986&partnerID=40&md5=610f27998c860a98fda1ee8d2d41a422 Ghanim, A.A.J. and Beddu, S. and Abd Manan, T.S.B. and Al Yami, S.H. and Irfan, M. and Mursal, S.N.F. and Mohd Kamal, N.L. and Mohamad, D. and Machmudah, A. and Yavari, S. and Mohtar, W.H.M.W. and Ahmad, A. and Rasdi, N.W. and Khan, T. (2022) Prediction of Runoff in Watersheds Located within Data-Scarce Regions. Sustainability (Switzerland), 14 (13). http://eprints.utp.edu.my/33363/
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Institutional Repository
url_provider http://eprints.utp.edu.my/
description The interest in the use of mathematical models for the simulation of hydrological processes has largely increased especially in the prediction of runoff. It is the subject of extreme research among engineers and hydrologists. This study attempts to develop a simple conceptual model that reflects the features of the arid environment where the availability of hydrological data is scarce. The model simulates an hourly streamflow hydrograph and the peak flow rate for any given storm. Hourly rainfall, potential evapotranspiration, and streamflow record are the significant input prerequisites for this model. The proposed model applied two (2) different hydrologic routing techniques: the time area curve method (wetted area of the catchment) and the Muskingum method (catchment main channel). The model was calibrated and analyzed based on the data collected from arid catchment in the center of Jordan. The model performance was evaluated via goodness of fit. The simulation of the proposed model fits both (a) observed and simulated streamflow and (b) observed and simulated peak flow rate. The model has the potential to be used for peak discharges� prediction during a storm period. The modeling approach described in this study has to be tested in additional catchments with appropriate data length in order to attain reliable model parameters. © 2022 by the authors. Licensee MDPI, Basel, Switzerland.
format Article
author Ghanim, A.A.J.
Beddu, S.
Abd Manan, T.S.B.
Al Yami, S.H.
Irfan, M.
Mursal, S.N.F.
Mohd Kamal, N.L.
Mohamad, D.
Machmudah, A.
Yavari, S.
Mohtar, W.H.M.W.
Ahmad, A.
Rasdi, N.W.
Khan, T.
spellingShingle Ghanim, A.A.J.
Beddu, S.
Abd Manan, T.S.B.
Al Yami, S.H.
Irfan, M.
Mursal, S.N.F.
Mohd Kamal, N.L.
Mohamad, D.
Machmudah, A.
Yavari, S.
Mohtar, W.H.M.W.
Ahmad, A.
Rasdi, N.W.
Khan, T.
Prediction of Runoff in Watersheds Located within Data-Scarce Regions
author_facet Ghanim, A.A.J.
Beddu, S.
Abd Manan, T.S.B.
Al Yami, S.H.
Irfan, M.
Mursal, S.N.F.
Mohd Kamal, N.L.
Mohamad, D.
Machmudah, A.
Yavari, S.
Mohtar, W.H.M.W.
Ahmad, A.
Rasdi, N.W.
Khan, T.
author_sort Ghanim, A.A.J.
title Prediction of Runoff in Watersheds Located within Data-Scarce Regions
title_short Prediction of Runoff in Watersheds Located within Data-Scarce Regions
title_full Prediction of Runoff in Watersheds Located within Data-Scarce Regions
title_fullStr Prediction of Runoff in Watersheds Located within Data-Scarce Regions
title_full_unstemmed Prediction of Runoff in Watersheds Located within Data-Scarce Regions
title_sort prediction of runoff in watersheds located within data-scarce regions
publisher MDPI
publishDate 2022
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85133551325&doi=10.3390%2fsu14137986&partnerID=40&md5=610f27998c860a98fda1ee8d2d41a422
http://eprints.utp.edu.my/33363/
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score 13.211869