Evaluation of statistical downscaling model's performance in projecting future climate change scenarios

被引:1
|
作者
Shukla, Rituraj [1 ]
Khare, Deepak [2 ]
Kumar Dwivedi, Anuj [3 ]
Rudra, Ramesh Pal [1 ]
Palmate, Santosh S. [4 ]
Ojha, C. S. P. [2 ]
Singh, Vijay P. [5 ,6 ]
机构
[1] Univ Guelph, Sch Engn, Guelph, ON, Canada
[2] Indian Inst Technol Roorkee, Roorkee, Uttarakhand, India
[3] Natl Inst Hydrol Roorkee, Roorkee, Uttarakhand, India
[4] Texas A&M Univ, El Paso Ctr, Texas A&M AgriLife Res, El Paso, TX USA
[5] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX USA
[6] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX USA
关键词
HadCM3; Indira Sagar Canal Command area; LS-SVM; SDSM; statistical downscaling;
D O I
10.2166/wcc.2023.207
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Statistical downscaling (SD) is preferable to dynamic downscaling to derive local-scale climate change information from large-scale datasets. Many statistical downscaling models are available these days, but comparison of their performance is still inadequately addressed for choosing a reliable SD model. Thus, it is desirable to compare the performance of SD models to ensure their adaptability in future climate studies. In this study, a statistical downscaling model (SDSM) or multi-linear regression and the Least Square Support Vector Machine (LS-SVM) were used to do downscaling and compare the results with those obtained from general circulation model (GCM) for identifying the best SD model for the Indira Sagar Canal Command area located in Madhya Pradesh, India. The GCM, Hadley Centre Coupled Model version 3 (HadCM3), was utilized to extract and downscale precipitation, maximum temperature (Tmax), and minimum temperature (Tmin) for 1961-2001 and then for 2001-2099. Before future projections, both SD models were initially calibrated (1961-1990) and validated (1991-2001) to evaluate their performance for precipitation and temperature variables at all gauge stations, namely Barwani, East Nimar, and West Nimar. Results showed that the precipitation trend was under-predicted owing to large errors in downscaling, while temperature was over-predicted by SD models.
引用
收藏
页码:3559 / 3595
页数:37
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