Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia

High resolution models from the High-Resolution Model Intercomparison Project (HighResMIP), part of CMIP6, have the capacity to allow a better representation of the climate system in tropical regions, but how different model resolutions affect hydrological outputs remains unclear. This research aims...

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Main Authors: Mou Leong Tan, Ju Liang, Matthew Hawcroft, James M. Haywood, Fei Zhang, Ruslan Rainis, Wan Ruslan Ismail
Format: Article
Language:English
Published: MDPI AG 2021-11-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/22/3158
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author Mou Leong Tan
Ju Liang
Matthew Hawcroft
James M. Haywood
Fei Zhang
Ruslan Rainis
Wan Ruslan Ismail
author_facet Mou Leong Tan
Ju Liang
Matthew Hawcroft
James M. Haywood
Fei Zhang
Ruslan Rainis
Wan Ruslan Ismail
author_sort Mou Leong Tan
collection DOAJ
description High resolution models from the High-Resolution Model Intercomparison Project (HighResMIP), part of CMIP6, have the capacity to allow a better representation of the climate system in tropical regions, but how different model resolutions affect hydrological outputs remains unclear. This research aims to evaluate projections of hydro-climatic change of the Johor River Basin (JRB) in southern Peninsular Malaysia between 1985 to 2015 and 2021 to 2050, focusing on uncertainty quantification of hydrological outputs from low (>1°), medium (0.5° to 1°) and high (≤0.5°) horizontal resolution models. These projections show future increases in annual precipitation of 0.4 to 3.1%, minimum and maximum temperature increases of 0.8 to 0.9 °C and 0.9 to 1.1 °C, respectively. These projected climate changes lead to increases in annual mean streamflow of 0.9% to 7.0% and surface runoff of 7.0% to 20.6% in the JRB. These annual mean changes are consistent with those during the wet period (November to December), e.g., streamflow increases of 4.9% to 10.8% and surface runoff of 28.8 to 39.9% in December. Disagreement in the direction of change is found during the dry seasons, (February to March and May to September), where high resolution models project a decrease in future monthly precipitation and streamflow, whilst increases are projected by the medium- and low-resolution models.
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spelling doaj.art-b5823dda335247d88492cfcbe4f917ce2023-11-23T01:59:14ZengMDPI AGWater2073-44412021-11-011322315810.3390/w13223158Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, MalaysiaMou Leong Tan0Ju Liang1Matthew Hawcroft2James M. Haywood3Fei Zhang4Ruslan Rainis5Wan Ruslan Ismail6GeoInformatic Unit, Geography Section, School of Humanities, Universiti Sains Malaysia (USM), Penang 11800, MalaysiaCollege of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QE, UKCentre for Applied Climate Sciences, University of Southern Queensland, Toowoomba, QLD 4350, AustraliaCollege of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QE, UKKey Laboratory of Wisdom City and Environmental Modeling of Higher Education Institute, College of Resources and Environment Sciences, Xinjiang University, Urumqi 830046, ChinaGeoInformatic Unit, Geography Section, School of Humanities, Universiti Sains Malaysia (USM), Penang 11800, MalaysiaGeoInformatic Unit, Geography Section, School of Humanities, Universiti Sains Malaysia (USM), Penang 11800, MalaysiaHigh resolution models from the High-Resolution Model Intercomparison Project (HighResMIP), part of CMIP6, have the capacity to allow a better representation of the climate system in tropical regions, but how different model resolutions affect hydrological outputs remains unclear. This research aims to evaluate projections of hydro-climatic change of the Johor River Basin (JRB) in southern Peninsular Malaysia between 1985 to 2015 and 2021 to 2050, focusing on uncertainty quantification of hydrological outputs from low (>1°), medium (0.5° to 1°) and high (≤0.5°) horizontal resolution models. These projections show future increases in annual precipitation of 0.4 to 3.1%, minimum and maximum temperature increases of 0.8 to 0.9 °C and 0.9 to 1.1 °C, respectively. These projected climate changes lead to increases in annual mean streamflow of 0.9% to 7.0% and surface runoff of 7.0% to 20.6% in the JRB. These annual mean changes are consistent with those during the wet period (November to December), e.g., streamflow increases of 4.9% to 10.8% and surface runoff of 28.8 to 39.9% in December. Disagreement in the direction of change is found during the dry seasons, (February to March and May to September), where high resolution models project a decrease in future monthly precipitation and streamflow, whilst increases are projected by the medium- and low-resolution models.https://www.mdpi.com/2073-4441/13/22/3158climate changeCMIP6HighResMIPSWATwater resourceresolution
spellingShingle Mou Leong Tan
Ju Liang
Matthew Hawcroft
James M. Haywood
Fei Zhang
Ruslan Rainis
Wan Ruslan Ismail
Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
Water
climate change
CMIP6
HighResMIP
SWAT
water resource
resolution
title Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
title_full Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
title_fullStr Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
title_full_unstemmed Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
title_short Resolution Dependence of Regional Hydro-Climatic Projection: A Case-Study for the Johor River Basin, Malaysia
title_sort resolution dependence of regional hydro climatic projection a case study for the johor river basin malaysia
topic climate change
CMIP6
HighResMIP
SWAT
water resource
resolution
url https://www.mdpi.com/2073-4441/13/22/3158
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