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Statistical downscaling of general circulation model outputs to precipitation accounting for non-stationarities in predictor-predictand relationships

机译:大气环流模型的统计降尺度输出到预测 - 预测关系中非平稳性的降水会计

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摘要

This paper presents a novel approach to incorporate the non-stationarities characterised in the GCM outputs, into the Predictor-Predictand Relationships (PPRs) in statistical downscaling models. In this approach, a series of 42 PPRs based on multi-linear regression (MLR) technique were determined for each calendar month using a 20-year moving window moved at a 1-year time step on the predictor data obtained from the NCEP/NCAR reanalysis data arcHIVe and observations of precipitation at 3 stations located in Victoria, Australia, for the period 1950-2010. Then the relationships between the constants and coefficients in the PPRs and the statistics of reanalysis data of predictors were determined for the period 1950-2010, for each calendar month. Thereafter, using these relationships with the statistics of the past data of HadCM3 GCM pertaining to the predictors, new PPRs were derived for the periods 1950-69, 1970-89 and 1990-99 for each station. This process yielded a non-stationary downscaling model consisting of a PPR per calendar month for each of the above three periods for each station. The non-stationarities in the climate are characterised by the long-term changes in the statistics of the climate variables and above process enabled relating the non-stationarities in the climate to the PPRs. These new PPRs were then used with the past data of HadCM3, to reproduce the observed precipitation. It was found that the non-stationary MLR based downscaling model was able to produce more accurate simulations of observed precipitation more often than conventional stationary downscaling models developed with MLR and Genetic Programming (GP).
机译:本文提出了一种新颖的方法,可以将GCM输出中表征的非平稳性纳入统计缩减模型中的Predictor-Predictand Relationships(PPR)。在这种方法中,使用从NCEP / NCAR获得的预测变量数据以1年时间步长移动的20年移动窗口,针对每个日历月确定了一系列基于多线性回归(MLR)技术的42个PPR。再分析数据arcHIVe和1950-2010年期间澳大利亚维多利亚州3个站点的降水观测。然后确定每个日历月在1950-2010年期间PPR中的常数和系数之间的关系以及预测变量的重新分析数据的统计数据。此后,利用这些关系以及与该预测变量有关的HadCM3 GCM的过去数据的统计信息,得出了每个电台1950-69、1970-89和1990-99期间的新PPR。此过程产生了一个非平稳的降尺度模型,该模型由每个日历的上述三个时段的每个日历月的PPR组成。气候中的非平稳性的特征是气候变量统计数据的长期变化,并且上述过程使得将气候中的非平稳性与PPR关联起来成为可能。然后将这些新的PPR与HadCM3的过去数据一起使用,以再现观测到的降水。发现基于非平稳MLR的降尺度模型比使用MLR和遗传编程(GP)开发的常规平稳降尺度模型能够更频繁地产生观测降水的模拟。

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