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首页> 外文期刊>Journal of Climate >Potential predictability of North American surface temperature. Part I: Information-based versus signal-to-noise-based metrics.
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Potential predictability of North American surface temperature. Part I: Information-based versus signal-to-noise-based metrics.

机译:北美表面温度的潜在可预测性。第一部分:基于信息与基于信噪比的指标。

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In this study, the potential predictability of the North American (NA) surface air temperature was explored using information-based predictability framework and Ensemble-Based Predictions of Climate Changes and their Impacts (ENSEMBLES) multiple model ensembles. Emphasis was put on the comparison of predictability measured by information-based metrics and by the conventional signal-to-noise ratio (SNR)-based metrics. Furthermore, the potential predictability was optimally decomposed into different modes by maximizing the predictable information (equivalent to the maximum of SNR), from which the most predictable structure was extracted and analyzed. It was found that the conventional SNR-based metrics underestimate the potential predictability, in particular in these areas where the predictable signals are relatively weak. The most predictable components of the NA surface air temperature can be characterized by the interannual variability mode and the long-term trend mode. The former is inherent to tropical Pacific sea surface temperature (SST) forcing such as El Nino-Southern Oscillation (ENSO), whereas the latter is closely associated with the global warming. The amplitude of the two modes has geographical variations in different seasons. On this basis, the possible physical mechanisms responsible for the predictable mode of interannual variability and its potential benefits to the improvement of seasonal climate prediction were discussed.
机译:在这项研究中,使用基于信息的可预测性框架和基于集合的气候变化及其影响预测(ENSEMBLES)多个模型集合,探索了北美(NA)地表气温的潜在可预测性。重点放在通过基于信息的度量标准和通过传统的基于信噪比(SNR)的度量标准对可预测性的比较上。此外,通过最大化可预测信息(等效于SNR的最大值),将潜在的可预测性最佳地分解为不同的模式,从中提取并分析最可预测的结构。发现传统的基于SNR的度量标准低估了潜在的可预测性,尤其是在可预测信号相对较弱的这些区域。 NA表面空气温度的最可预测成分可以通过年际变化模式和长期趋势模式来表征。前者是热带太平洋海表温度(SST)强迫所固有的,例如厄尔尼诺-南方涛动(ENSO),而后者与全球变暖密切相关。两种模式的振幅在不同季节具有地理差异。在此基础上,讨论了造成年际变化可预测模式的可能物理机制及其对改善季节气候预测的潜在好处。

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