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Summer high temperature extremes over Northeastern China predicted by spring soil moisture

机译:夏季高温极端东北地区春天土壤水分预测

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Current seasonal climate predictions mainly reside in the ocean anomalies. However, the prediction skills are generally limited over many extra-tropical land areas where the oceanic effects are relatively weak. In this study, we address the potential of preceding spring soil moisture condition to predict summer hot days over Northeastern China, a typical Northern Hemisphere mid-latitude region. The results show that spring soil moisture condition over Central-Eastern China is closely related with following summer hot days over Northeastern China for the period of 1979-2017. The statistical model based on the preceding spring soil moisture condition yields temporal cross-validated correlation skill of 0.57 for summer hot days over Northeastern China. The spatial pattern correlation skills of independent hindcast experiments for 2009-2017 are also high, ranging from 0.87 to 0.94. Our results can be easily applied to practical prediction of summer hot days over Northeastern China, and help to provide better climate services and reduce the detrimental effects of extreme heat over this extra-tropical region.
机译:目前的季节性气候预测主要位于海洋异常中。然而,预测技能通常限制在许多额外热带地区,海洋效应相对较弱。在这项研究中,我们解决了春天土壤水分状况的潜力,以预测中国东北部的夏季炎热日,典型的北半球中纬度地区。结果表明,中国中央东部的春天土壤水分状况与东北东北炎在中国东北部1979 - 2017年的炎热日子密切相关。基于春季土壤湿度条件的统计模型在中国东北夏季炎热日将0.57的时间交叉验证相关技术产量为0.57。 2009 - 2017年独立的Hindcast实验的空间模式相关技能也高,范围为0.87至0.94。我们的结果可以轻松应用于中国东北夏季炎热日的实际预测,并有助于提供更好的气候服务,并降低极端热量对这种额外热带地区的不利影响。

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