2010
DOI: 10.3354/cr00835
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Upgrades to the reliability ensemble averaging method for producing probabilistic climate-change projections

Abstract: We present an augmented version of the reliability ensemble averaging (REA) method designed to generate probabilistic climate-change information from ensembles of climate model simulations. Compared to the original version, the augmented method includes consideration of multiple variables and statistics in the calculation of performance-based weighting. In addition, the model convergence criterion previously employed has been removed. The method is applied to the calculation of changes in mean values and the v… Show more

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Cited by 143 publications
(131 citation statements)
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References 17 publications
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“…3b,c). For DJF, the results from both experiments exhibit a bias toward cold temperatures over land areas, as in previous studies (e.g., Zhang et al 2008;Xu et al 2010;Lee et al 2013). However, those from the RSM show an improved pattern by reducing the cold biases although a distinct cold bias over the Tibetan Plateau region is aggravated by the RSM downscaling (cf.…”
Section: Evaluation Of Current Climate Simulationsupporting
confidence: 67%
“…3b,c). For DJF, the results from both experiments exhibit a bias toward cold temperatures over land areas, as in previous studies (e.g., Zhang et al 2008;Xu et al 2010;Lee et al 2013). However, those from the RSM show an improved pattern by reducing the cold biases although a distinct cold bias over the Tibetan Plateau region is aggravated by the RSM downscaling (cf.…”
Section: Evaluation Of Current Climate Simulationsupporting
confidence: 67%
“…This approach has been used in multiple examinations of both global and regional climate model results (Sobolowski and Pavelsky 2012), and as a point of departure for formulating probability density functions (Tebaldi and Knutti 2007). More recently the method has been revised to dispense with the model convergence criterion (Xu et al 2010), which has been controversial in some quarters.…”
Section: Assigning Different Weights To Each Model In a Multi-model Ementioning
confidence: 99%
“…The overestimation of precipitation around regions with steep orography is an evident instance of such systematic model errors in current state-of-the-art GCMs (e.g., Su et al 2013;Mehran et al 2014). The ensemble of Coupled Model Intercomparison Project Phase 3 (CMIP3) models overestimates the amount of precipitation over the Tibetan Plateau by up to 100 % (Xu et al 2010). This is also true for other regions with high mountains, e.g., the Andes mountains, where both regional and global models tend to produce excessive precipitation (Alves and Marengo 2010;Gulizia and Camilloni 2015).…”
Section: Introductionmentioning
confidence: 99%