Projections of Future Climate Change in the Vu Gia Thu Bon River Basin, Vietnam by Using Statistical DownScaling Model (SDSM)

被引:22
作者
Dang Nguyen Dong Phuong [1 ]
Trung Q Duong [2 ]
Nguyen Duy Liem [3 ]
Vo Ngoc Quynh Tram [1 ]
Dang Kien Cuong [4 ]
Nguyen Kim Loi [1 ]
机构
[1] Nong Lam Univ Ho Chi Minh City, Res Ctr Climate Change, Ho Chi Minh City 700000, Vietnam
[2] Queens Univ Belfast, Sch Elect Elect Engn & Comp Sci, Belfast BT7 1NN, Antrim, North Ireland
[3] Nong Lam Univ Ho Chi Minh City, Fac Environm & Nat Resources, Ho Chi Minh City 700000, Vietnam
[4] Nong Lam Univ Ho Chi Minh City, Fac Informat Technol, Ho Chi Minh City 700000, Vietnam
关键词
climate change; climate projection; SDSM; Vu Gia Thu Bon river basin; GENERAL-CIRCULATION MODEL; UNCERTAINTY ANALYSIS; EXTREME RAINFALL; REFINED INDEX; LARS-WG; TEMPERATURE; PRECIPITATION; IMPACTS; EVENTS; PERFORMANCE;
D O I
10.3390/w12030755
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Future projections of anthropogenic climate change play a pivotal role in devising viable countermeasures to address climate-related risks. This study strove to construct future daily rainfall and maximum and minimum temperature scenarios in Vu Gia Thu Bon river basin by employing the Statistical DownScaling Model (SDSM). The model performance was evaluated by utilizing a Taylor diagram with dimensioned and dimensionless statistics. During validation, all model-performance measures show good ability in simulating extreme temperatures and reasonable ability for rainfall. Subsequently, a set of predictors derived from HadCM3 and CanESM2 was selected to generate ensembles of each climatic variables up to the end of 21st century. The generated outcomes exhibit a consistent increase in both extreme temperatures under all emission scenarios. The greatest changes in maximum and minimum temperature were predicted to increase by 2.67-3.9 degrees C and 1.24-1.96 degrees C between the 2080s and reference period for the worst-case scenarios. Conversely, there are several discrepancies in the projections of rainfall under different emission scenarios as well as among considered stations. The predicted outcomes indicate a significant decrease in rainfall by approximately 11.57%-17.68% at most stations by 2099. Moreover, all ensemble means were subjected to the overall and partial trend analysis by applying the Innovative-Sen trend analysis method. The results exhibit similar trend patterns, thereby indicating high stability and applicability of the SDSM. Generally, it is expected that these findings will contribute numerous valuable foundations to establish a framework for the assessment of climate change impacts at the river basin scale.
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页数:17
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