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A Proposed Downscaling Model for Climate Change Studies

机译:拟议的降尺度模型用于气候变化研究

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General Circulation Models (GCMs) are commonly used to simulate future climate conditions in climate change studies. However the resolution from these models is too coarse for river basin scale studies. As such the results from these models need to be downscaled appropriately for use at the basin scale. Well known downscaling models include various dynamical and statistical approaches. However, none of these has been officially recommended as the best model for use in all regions. Disadvantages of existing downscaling models include high cost of operation, inability to avoid producing unrealistic values, inability to include multiple variables, and inability to reflect the future change of variability. In this paper, the development of a new downscaling model is based on a hybrid of algebraic and stochastic approaches that can include multiple variables is proposed. This new model will be called the HYAS model. HYAS employs the differences between simulated future and baseline variables added to simulated changing residual variance. This new approach has been applied in a climate change study of the Jangkok River Basin in Lombok, Indonesia. Twenty years (1971 to 1990) of GCM outputs were set as baseline variables and were used in the calibration process. The subsequent, twenty years (1991 to 2010) of data were used for model validation. Then, the relevant GCM outputs from 2011 to 2100 were used as model predictors to simulate the following regional climatic variables: humidity, rainfall, sunshine, temperature, and wind speed. Results showed that the following GCM variables: Screen 2m Temperature, Screen Specific Humidity, and Skin Temperature are appropriate for modeling regional humidity, rainfall, sunshine, and air temperature. However for modelling regional wind speed, the following GCM variables: Evaporation, Screen 2m Temperature, and Surface Pressure are more appropriate. The HYAS model is found to be superior to existing methods for predicting regional climatic variables in the Jangkok River Basin.
机译:通用循环模型(GCM)通常用于模拟气候变化研究中的未来气候条件。但是,这些模型的分辨率对于流域规模研究而言过于粗糙。因此,这些模型的结果需要适当缩小以用于流域规模。众所周知的缩减模型包括各种动态和统计方法。但是,这些都没有被正式推荐为在所有地区都可以使用的最佳模型。现有缩减模型的缺点包括操作成本高,无法避免产生不现实的值,无法包含多个变量以及无法反映未来的可变性变化。在本文中,提出了一种新的降尺度模型,该模型基于代数和随机方法的混合,可以包含多个变量。这个新模型将被称为HYAS模型。 HYAS利用模拟的未来变量和基准变量之间的差异,将其添加到模拟的变化残差中。这种新方法已应用于印度尼西亚龙目岛Jangkok流域的气候变化研究中。 GCM输出的二十年(1971年至1990年)被设置为基线变量,并用于校准过程。随后的二十年(1991年至2010年)数据用于模型验证。然后,将2011年至2100年的相关GCM产出用作模型预测指标,以模拟以下区域气候变量:湿度,降雨量,日照,温度和风速。结果表明,以下GCM变量:屏幕2m温度,屏幕特定湿度和皮肤温度适用于对区域湿度,降雨,日照和空气温度进行建模。但是,对于建模区域风速,以下GCM变量更合适:蒸发,屏幕2m温度和表面压力。人们发现,HYAS模型优于现有的用于预测江角流域区域气候变量的方法。

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