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Combination of Multimodel Probabilistic Forecasts Using an Optimal Weighting System

机译:使用最优加权系统的多模型概率预测的组合

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In this study, an optimal weighting system is developed that combines multiple seasonal probabilistic forecasts in the North American Multimodel Ensemble (NMME). The system is applied to predict temperature and precipitation over the North American continent, and the analysis is conducted using the 1982-2010 hindcasts from eight NMME models, including the CFSv2, CanCM3, CanCM4, GFDL CM2.1, Forecast-Oriented Low Ocean Resolution (FLOR), GEOS5, CCSM4, and CESM models, with weights determined by minimizing the Brier score using ridge regression. Strategies to improve the performance of ridge regression are explored, such as eliminating a priori models with negative skill and increasing the effective sample size by pooling information from neighboring grids. A set of constraints is put in place to confine the weights within a reasonable range or restrict the weights from departing wildly from equal weights. So when the predictor-predictand relationship is weak, the multimodel ensemble forecast returns to an equal-weight combination. The new weighting system improves the predictive skill from the baseline, equally weighted forecasts. All models contribute to the weighted forecasts differently based upon location and forecast start and lead times. The amount of improvement varies across space and corresponds to the average model elimination percentage. The areas with higher elimination rates tend to show larger improvement in cross-validated verification scores. Some local improvements can be as large as 0.6 in temporal probability anomaly correlation (TPAC). On average, the results are about 0.02-0.05 in TPAC for temperature probabilistic forecasts and 0.03-0.05 for precipitation probabilistic forecasts over North America. The skill improvement is generally greater for precipitation probabilistic forecasts than for temperature probabilistic forecasts.
机译:在这项研究中,开发了一种最佳加权系统,其结合了北美多模块集合(NMME)的多个季节性概率预测。该系统应用于预测北美大陆的温度和降水,并使用来自八个NMME模型的1982-2010 HindCasts进行分析,包括CFSv2,CANM3,CANM4,GFDL CM2.1预测导向的低海洋分辨率(Flor),Geos5,CCSM4和CESM模型,通过使用脊回归最小化Brizer分数来确定权重。探索了提高脊回归性能的策略,例如消除具有负技能的先验模型,并通过从相邻网格中汇集信息来增加有效的样本大小。放置一组约束,以限制合理范围内的重量,或限制从相等权重离开野外的权重。因此,当预测器预测和关系较弱时,多模型集合预测返回到相等重量的组合。新的加权系统改善了基线的预测技能,同样加权预测。基于位置和预测开始和交货时间,所有型号的所有型号都有助于不同的预测。改善量越差地越差,并且对应于平均模型消除百分比。具有更高率率较高的区域倾向于显示交叉验证验证评分的更大改善。在时间概率异常相关性(TPAC)中,一些局部改进可以大约0.6。平均而言,在TPAC中,结果为0.02-0.05,对于温度概率预测,0.03-0.05在北美的降水概率预测。降水概率预测的技能改善通常更大,而不是温度概率预测。

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