Projected temperature and precipitation changes using the LARS-WG statistical downscaling model in the Shire River Basin, Malawi
Sheila Kavwenje
School of Environmental Science and Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Data curation, Formal analysis, Funding acquisition, Investigation, Methodology, Resources, Visualization, Writing - original draft, Writing - review & editing
Search for more papers by this authorCorresponding Author
Lin Zhao
School of Environmental Science and Engineering, Tianjin University, Tianjin, China
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
Correspondence
Lin Zhao, School of Environmental Science and Engineering, Tianjin University, Tianjin 300072, China.
Email: [email protected]
Contribution: Conceptualization, Resources, Supervision, Validation
Search for more papers by this authorLiang Chen
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
School of Civil Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Formal analysis, Methodology, Supervision, Validation, Writing - review & editing
Search for more papers by this authorEvance Chaima
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
School of Civil Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Formal analysis, Investigation, Methodology, Validation, Visualization
Search for more papers by this authorSheila Kavwenje
School of Environmental Science and Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Data curation, Formal analysis, Funding acquisition, Investigation, Methodology, Resources, Visualization, Writing - original draft, Writing - review & editing
Search for more papers by this authorCorresponding Author
Lin Zhao
School of Environmental Science and Engineering, Tianjin University, Tianjin, China
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
Correspondence
Lin Zhao, School of Environmental Science and Engineering, Tianjin University, Tianjin 300072, China.
Email: [email protected]
Contribution: Conceptualization, Resources, Supervision, Validation
Search for more papers by this authorLiang Chen
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
School of Civil Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Formal analysis, Methodology, Supervision, Validation, Writing - review & editing
Search for more papers by this authorEvance Chaima
State Key Laboratory of Hydraulic Engineering Simulation and Safety, Tianjin University, Tianjin, China
School of Civil Engineering, Tianjin University, Tianjin, China
Contribution: Conceptualization, Formal analysis, Investigation, Methodology, Validation, Visualization
Search for more papers by this authorFunding information: National Key R&D Program of China, Grant/Award Number: 2016YFC0401405; Tianjin Science and Technology Plan Project, Grant/Award Number: 18ZXSZSF00240
Abstract
This study analyzes local-scale temperature and precipitation projections in the Shire River Basin (SRB) in Malawi using 10 global circulation models (GCMs) available in the coupled model intercomparison project phase 5 (CMIP5), under two representative concentration pathways (RCP 4.5 and RCP 8.5). For nine stations in the study area, large-scale maximum temperature (Tmax), minimum temperature (Tmin) and precipitation data from the selected GCMs were downscaled by the sixth version of the Long Ashton Research Station Weather Generator (LARS-WG6). The mean seasonal and annual change projections for Tmax, Tmin and precipitation during two future periods, that is, the middle future (2041–2070) and late future (2071–2100) periods were analyzed. Modelling results demonstrated that the LARS-WG model is capable of simulating temperature more accurately than precipitation in the SRB. All 10 GCMs revealed that continually rising temperatures are anticipated in the study area; however, the projected magnitude of change varied across GCMs and between RCPs. Generally, the increase in average Tmax and Tmin was observed to be higher under RCP 8.5 compared with RCP 4.5 due to unmitigated greenhouse gas emissions (GHGs). Future precipitation change results showed more complexity and uncertainty than for temperature; not all GCMs agree on whether there will be positive or negative changes in precipitation and no systematic variations under RCP4.5 and RCP8.5 were observed during the two future time period, illustrating that both GCMs and RCPs are important sources of the relatively large uncertainties in future precipitation projections in the SRB. Thus, this study indicated that uncertainties constrained by both GCMs and RCPs are crucial and need to always be considered when executing climate impact studies and adaptation, particularly at river basin level.
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