Downscaling of Precipitation for Lake Catchment in Arid Region in India using Linear Multiple Regression and Neural Networks

C. Ojha, M. Goyal, A. Adeloye
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引用次数: 33

Abstract

In this paper, downscaling models are developed using a Linear Multiple Regression (LMR) and Artificial Neural Networks (ANNs) for obtaining projections of mean monthly precipitation to lake-basin scale in an arid region in India. The effectiveness of these techniques is demonstrated through application to downscale the predictand (precipita- tion) for the Pichola lake region in Rajasthan state in India, which is considered to be a climatically sensitive region. The predictor variables are extracted from (1) the National Centers for Environmental Prediction (NCEP) reanalysis dataset for the period 1948-2000, and (2) the simulations from the third-generation Canadian Coupled Global Climate Model (CGCM3) for emission scenarios A1B, A2, B1 and COMMIT for the period 2001-2100. The scatter plots and cross- correlations are used for verifying the reliability of the simulation of the predictor variables by the CGCM3. The perform- ance of the linear multiple regression and ANN models was evaluated based on several statistical performance indicators. The ANN based models is found to be superior to LMR based models and subsequently, the ANN based model is applied to obtain future climate projections of the predictand (i.e precipitation). The precipitation is projected to increase in future for A2 and A1B scenarios, whereas it is least for B1 and COMMIT scenarios using predictors. In the COMMIT scenario, where the emissions are held the same as in the year 2000.
基于线性多元回归和神经网络的印度干旱区湖泊集水区降水降尺度研究
本文利用线性多元回归(LMR)和人工神经网络(ANNs)建立了降尺度模型,用于获得印度干旱区月平均降水到湖-流域尺度的预估。这些技术的有效性通过应用于印度拉贾斯坦邦Pichola湖地区的降水预测(降水)的缩小尺度得到了证明,该地区被认为是一个气候敏感地区。预测变量提取自(1)美国国家环境预测中心(NCEP) 1948-2000年再分析数据集和(2)第三代加拿大耦合全球气候模式(CGCM3)对2001-2100年A1B、A2、B1和COMMIT排放情景的模拟。利用散点图和相互关系验证了CGCM3对预测变量模拟的可靠性。基于几个统计性能指标对线性多元回归和人工神经网络模型的性能进行了评价。基于人工神经网络的模式被发现优于基于LMR的模式,随后,基于人工神经网络的模式被应用于预测物(即降水)的未来气候预测。使用预测器预估未来A2和A1B情景的降水会增加,而B1和COMMIT情景的降水最少。在COMMIT情景中,排放量保持与2000年相同。
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