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Projection the long-term ungauged rainfall using integrated Statistical Downscaling Model and Geographic Information System (SDSM-GIS) model

机译:使用统计降尺度模型和地理信息系统(SDSM-GIS)模型来预测长期未降雨

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摘要

An accuracy in the hydrological modelling will be affected when having limited data sources especially at ungauged areas. Due to this matter, it will not receiving any significant attention especially on the potential hydrologic extremes. Thus, the objective was to analyse the accuracy of the long-term projected rainfall at ungauged rainfall station using integrated Statistical Downscaling Model and Geographic Information System (SDSM-GIS) model. The SDSM was used as a climate agent to predict the changes of the climate trend in Δ2030s by gauged and ungauged stations. There were five predictors set have been selected to form the local climate at the region which provided by NCEP (validated) and CanESM2-RCP4.5 (projected). According to the statistical analyses, the SDSM was controlled to produce reliable validated results with lesser %MAE (<23%) and higher R. The projected rainfall was suspected to decrease 14% in Δ2030s. All the RCPs agreed the long term rainfall pattern was consistent to the historical with lower annual rainfall intensity. The RCP8.5 shows the least rainfall changes. These findings then used to compare the accuracy of monthly rainfall at control station (Stn 2). The GIS-Kriging method being as an interpolation agent was successfully to produce similar rainfall trend with the control station. The accuracy was estimated to reach 84%. Comparing between ungauged and gauged stations, the small %MAE in the projected monthly results between gauged and ungauged stations as a proved the integrated SDSM-GIS model can producing a reliable long-term rainfall generation at ungauged station.
机译:当数据来源有限时,尤其是在未开垦的地区,水文建模的准确性会受到影响。由于这个问题,它将不会受到任何特别的关注,尤其是在潜在的水文极端事件上。因此,目的是使用集成的统计降尺度模型和地理信息系统(SDSM-GIS)模型来分析非持续降雨站的长期预计降雨的准确性。 SDSM被用作气候因子,通过有序站和无轨站预测Δ2030年代气候趋势的变化。已经选择了五个预测因子集以形成由NCEP(已验证)和CanESM2-RCP4.5(已预测)提供的区域的局部气候。根据统计分析,控制SDSM以产生可靠的经过验证的结果,其%MAE(<23%)和R较高。怀疑Δ2030s中的预计降雨量减少了14%。所有RCP都同意长期降雨模式与历史一致,年降雨量较低。 RCP8.5显示的降雨量最小。然后将这些发现用于比较控制站(Stn 2)每月降雨的准确性。 GIS-Kriging方法作为插值代理成功地产生了与控制站相似的降雨趋势。准确性估计达到84%。比较未测量站和已测量站之间,已测量站和未测量站之间的每月预测结果中的%MAE较小,这证明集成的SDSM-GIS模型可以在未测量站产生可靠的长期降雨。

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