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Southeastern United States summer rainfall framework and its implication for?seasonal prediction

机译:美国东南部夏季降水框架及其对季节预报的启示

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A new rainfall framework is constructed to describe the complex probability distribution of southeastern United States (SE US) summer (June–July–August) rainfall, which cannot be well represented by traditional kernel fitting methods. The new framework is based on the configuration of a three-cluster finite normal mixture model and is realized by Bayesian inference and a Markov Chain Monte Carlo (MCMC) algorithm. The three rainfall clusters reflect the probability distribution of light, moderate, and heavy rainfall in summer, and are linked to different climate factors. The variation of light rainfall intensity is likely associated with the combined effects of La Ni?a and the tri-pole sea surface temperature anomaly (SSTA) over the North Atlantic. Heavy rainfall concurs with a 'horseshoe-like' SSTA over the North Atlantic. In contrast, moderate rainfall is less correlated with the SSTA and likely caused by atmospheric internal dynamics. Rainfall characteristics and their linkages with SSTAs help improve seasonal predictions of regional climate. Such a new framework has an important implication in understanding the response of regional hydrology to climate variability and climate change; and our study suggest that it can be extended to other regions and seasons with similar climate.
机译:构建了一个新的降雨框架来描述美国东南部(SE US)夏季(6月至7月至8月)降雨的复杂概率分布,而传统的核拟合方法无法很好地表示这种降雨。新框架基于三簇有限正态混合模型的配置,并通过贝叶斯推理和马尔可夫链蒙特卡洛(MCMC)算法实现。这三个降雨群反映了夏季轻,中,强降雨的概率分布,并且与不同的气候因素有关。降雨强度的变化可能与La Ni?a和北大西洋三极海面温度异常(SSTA)的综合影响有关。大雨与北大西洋上空的“马蹄形” SSTA一致。相反,中度降雨与SSTA的相关性较小,可能是由大气内部动力学引起的。降雨特征及其与SSTA的联系有助于改善区域气候的季节性预测。这种新的框架对理解区域水文学对气候变化和气候变化的反应具有重要意义;我们的研究表明,它可以扩展到气候相似的其他地区和季节。

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