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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Development of a time‐varying downscaling model considering non‐stationarity using a Bayesian approach
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Development of a time‐varying downscaling model considering non‐stationarity using a Bayesian approach

机译:使用贝叶斯方法考虑非公平性的时变缩小模型的发展

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> Stationarity in the relationship between causal variables and target variables is the fundamental assumption of statistical downscaling models. However, we hypothesize that this assumption may not be valid in a changing climate. This study develops a downscaling technique in which the relationship between causal and target variables is considered to be time‐varying rather than static. The proposed time‐varying downscaling model (TVDM) is utilized to downscale monthly precipitation over India to 0.25 × 0.25° gridded scale using the large‐scale outputs from multiple general circulation models (GCMs), namely the Hadley Centre Coupled Model version 3 (HadCM3), coupled Hadley Centre Global Environmental Model version 2‐Earth System model (HadGEM2‐ES) and Canadian Earth System Model version 2 (CanESM2). Observed precipitation data are obtained from the India Meteorological Department (IMD), Pune. For future projection, the temporal evolution of each of the TVDM parameters is investigated using its deterministic (trend and periodicity) and stochastic components. TVDM is found to outperform the most commonly used statistical downscaling model (SDSM) and regional climate model (RCM) output at all the locations. The Regional Climate Model version 4 (RegCM4) precipitation data (RCM outputs) are obtained from the Coordinated Regional Climate Downscaling Experiment (CORDEX) data portal supplied by Indian Institute of Tropical Meteorology (IITM), Pune. The proposed model (TVDM) differs from the existing stationarity assumption‐based approaches in updating the relationship between causal and target variables over time. It is understood that parameter uncertainty is the major issue in consideration of non‐stationarity. Still, the TVDM is found to be very useful in the context of climate change due to its time‐varying comp
机译: >在因果变量和目标变量之间的关系中的pathtarity是基本的假设统计缩小模型。然而,我们假设这种假设在不断变化的气候中可能无效。本研究开发了一种缩小技术,其中因果关系和目标变量之间的关系被认为是时变而不是静态。使用多个通用循环模型(GCMS)的大规模输出,所提出的时变缩小模型(TVDM)用于将每月降水量降低到0.25×0.25°的网格秤,即Hadley中心耦合型号3(HADCM3 ),耦合Hadley中心全球环境模型版本2地球系统模型(Hadgem2-es)和加拿大地球系统模型版本2(Canesm2)。观察到的降水数据是从印度气象部门(IMD),浦那获得的。对于未来的投影,使用其确定性(趋势和周期性)和随机分量来研究每个TVDM参数的时间演变。 DVDM被发现以满足所有地点的最常用统计缩小模型(SDSM)和区域气候模型(RCM)输出。区域气候模型版本4(REGCM4)降水数据(RCM产出)是从印度热带气象(IITM),浦那提供的协调区域气候缩小实验(CORDEX)数据门户。所提出的模型(TVDM)与现有的基于实体定义的方法不同,在更新因果关系和目标变量之间的关系时。据了解,参数不确定性是考虑非公平性的主要问题。尽管如此,TVDM仍然被认为在气候变化的背景下非常有用,因为它时变 comp

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