印度中央邦英迪拉萨加尔运河指挥区降雨和温度气候变化情景的统计降尺度

Rituraj, Shukla
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引用次数: 15

摘要

一般环流模式(GCMs)已被气候机构用于预测未来气候变化。GCM输出局部相关性的一个具有挑战性的问题是它们对投影变量的粗糙空间分辨率。统计降尺度模型(SDSM)识别大尺度预测因子(即基于gcm的)和使用多元线性回归模型的局部尺度预测因子之间的关系。本研究将SDSM应用于gcm的小尺度降水和温度。位于印度中央邦英迪拉萨加尔运河指挥区的单个站点的数据被用作SDSM的输入。该研究包括对包括NCEP再分析数据在内的大尺度大气变量的校准和验证,以及基于气候情景的未来估算,即HadCM3 A2。降尺度实验结果表明,在定标和验证阶段,SDSM模型在日降雨量和温度降尺度方面的表现是可以接受的。在未来一段时期(2010-2099年),SDSM模式估计了该站年平均总降雨量和年平均气温的增加。这表明所考虑的站点区域在未来将是潮湿的。同时,预计目前研究区域的平均气温将上升至1.5℃至2.5℃。然而,模式预估显示,在HadCM3模式A2下,7月(0.59% ~ 2.09%)和8月(0.79% ~ 1.19%)的日平均降水量在未来时期有不同百分比的增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Statistical Downscaling of Climate Change Scenarios of Rainfall and Temperature over Indira Sagar Canal Command Area in Madhya Pradesh, India
General circulation models (GCMs) have been employed by climate agencies to predict future climate change. A challenging issue with GCM output for local relevance is their coarse spatial resolution of the projected variables. Statistical Downscaling Model (SDSM) identifies relationships between large-scale predictors (i.e., GCM-based) and local-scale predictands using multiple linear regression models. In this study (SDSM) was applied to downscale rainfall and temperature from GCMs. The data from single station located in the Indira Sagar canal command area at Madhya Pradesh, India were used as input of the SDSM. The study included calibration and validation with large-scale atmospheric variables encompassing the NCEP reanalysis data, the future estimation due to a climate scenario, which is HadCM3 A2. Results of the downscaling experiment demonstrate that during the calibration and validation stages, the SDSM model can be well acceptable regard its performance in the downscaling of daily rainfall and temperature. For a future period (2010-2099), the SDSM model estimated an increase in total average annual rainfall and annual average temperature for station. This indicates that the area of station considered will be wet and humid in the future. Also, the mean temperature is projected to rise to 1.5 C to 2.5 C for present study area. However, the model projections show a rise in mean daily precipitation with varying percentage in the months of July (0.59% to 2.09%) and August (0.79% to 1.19) under A2 of HadCM3 model for future periods.
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