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A copula-based precipitation forecasting model: Investigating the interdecadal modulation of ENSO's impacts on monthly precipitation

机译:基于copula的降水预测模型:调查ENSO对月降水的影响的年代际调制

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[1] The influence of two large-scale circulation patterns (the El Nino Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO)), and the effect of the interdecadal modulation of ENSO on precipitation in the state of Texas, U.S., was explored. Texas, by virtue of its size, topography, and geographical location, spans a wide range of climatic regions. The state is divided into 10 climate divisions. The precipitation pattern in each division follows different probability distributions. The climate regimes which trigger this difference are discussed. The seasonal correlation between ENSO and PDO with precipitation anomaly in each climate division was established. Copula-based models were developed to examine the dependence structure between the large-scale climate indices and average monthly seasonal precipitation. The choice of copula is discussed in light of the dependence structure. The selected copulas were then used to simulate precipitation anomalies in three climate divisions: one which has a semiarid climate, one located in the wettest region, and one straddling the subtropical humid and subtropical subhumid regions of the state. The statistical performance of bivariate models for ENSO and precipitation, and trivariate models for ENSO, PDO, and precipitation, in simulating precipitation anomalies were compared. In general, inclusion of PDO was found to improve simulation results. The most notable improvement was in simulating negative precipitation anomalies during La Nina and negative PDO. The copula models were also tested for their abilities to predict precipitation anomalies in these three regions. Again, the trivariate models performed better, especially in predicting droughts due to La Nina and negative PDO.
机译:[1]两种大规模的环流模式(厄尔尼诺南方涛动(ENSO)和太平洋年代际涛动(PDO))的影响,以及ENSO年代际调制对美国德克萨斯州降水的影响,被探索了。得克萨斯州凭借其规模,地形和地理位置,涵盖了广泛的气候区域。该州分为10个气候区。每个分区的降水模式遵循不同的概率分布。讨论了引发这种差异的气候体制。建立了每个气候区ENSO和PDO与降水异常之间的季节相关性。开发了基于Copula的模型,以检查大规模气候指数与平均每月季节性降水之间的依存关系。根据依赖性结构讨论了copula的选择。然后,使用选定的copulas模拟三个气候分区的降水异常:一个分区为半干旱气候,一个分区位于最湿润的地区,另一个跨越该州的亚热带湿润和亚热带亚湿润地区。比较了ENSO和降水的双变量模型以及ENSO,PDO和降水的三变量模型在模拟降水异常中的统计性能。通常,发现包含PDO可以改善仿真结果。最显着的改进是模拟了拉尼娜期间的负降水异常和负PDO。还测试了copula模型预测这三个区域降水异常的能力。同样,三变量模型的效果更好,尤其是在预测由于拉尼娜和负PDO造成的干旱方面。

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  • 来源
    《Water resources research》 |2014年第1期|580-600|共21页
  • 作者单位

    Water Management and Hydrological Science, 321E Scoates Hall, MS 2117, Texas A&M University, College Station, TX 77843, USA;

    Glenn Department of Civil Engineering, Clemson University, Clemson, South Carolina, USA;

    Water Management and Hydrological Science, Texas A&M University, College Station, Texas, USA,Department of Biological and Agricultural Engineering, Texas A&M University, College Station, Texas, USA,Zachry Department of Civil Engineering, Texas A&M University, College Station, Texas, USA;

    Water Management and Hydrological Science, Texas A&M University, College Station, Texas, USA,Department of Geology and Geophysics, Texas A&M University, College Station, Texas, USA;

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