Sachindra D A, Perera B J C
Institute for Sustainability and Innovation, College of Engineering and Science Victoria University, Melbourne, Victoria, Australia.
PLoS One. 2016 Dec 20;11(12):e0168701. doi: 10.1371/journal.pone.0168701. eCollection 2016.
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).
本文提出了一种新方法,将全球气候模式(GCM)输出中所表征的非平稳性纳入统计降尺度模型中的预测因子-预测对象关系(PPR)。在这种方法中,对于1950 - 2010年期间,利用从NCEP/NCAR再分析数据存档中获取的预测因子数据以及澳大利亚维多利亚州3个站点的降水观测数据,以1年时间步长移动的20年滑动窗口,为每个日历月确定了一系列基于多元线性回归(MLR)技术的42个PPR。然后确定了1950 - 2010年期间每个日历月PPR中的常数和系数与预测因子再分析数据统计量之间的关系。此后,利用这些与HadCM3 GCM预测因子过去数据统计量的关系,为每个站点推导出了1950 - 69年、1970 - 89年和1990 - 99年期间的新PPR。这一过程产生了一个非平稳降尺度模型,该模型由上述三个时期中每个时期每个站点的每个日历月的一个PPR组成。气候中的非平稳性通过气候变量统计量的长期变化来表征,上述过程使得能够将气候中的非平稳性与PPR联系起来。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。结果发现,基于非平稳MLR的降尺度模型比使用MLR和遗传规划(GP)开发的传统平稳降尺度模型更频繁地能够对观测到的降水进行更准确的模拟。