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Diagnosis of the Tropical Moisture Exports to the Mid-Latitudes and the Role of Atmospheric Steering in the Extreme Precipitation

机译:向中纬度地区输出热带水分的诊断及大气转向在极端降水中的作用

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Three river basins, i.e., the Yangtze river, the Mississippi river and the Loire river, were presented as case studies to explore the association among atmospheric circulations, moisture exports and extreme precipitations in the mid-latitudes. The major moisture source regions in the tropics for the three river basins are first identified using the Tropical Moisture Exports (TMEs) dataset. The space-time characteristics of their respective moisture sources are presented. Then, the trajectory curve clustering analysis is applied to the TMEs tracks originating from the identified source regions during each basin?¢????s peak TMEs activity and flood seasons. Our results show that the moisture tracks for each basin can be categorized into 3 or 4 clusters with distinct spatial trajectory features. Our further analysis on these clustered trajectories reveals that the contributions of moisture release from different clusters are associated with their trajectory features and travel speeds. In order to understand the role of associated atmospheric steering, daily composites of the geopotential heights anomalies and the vertical integral of moisture flux anomalies from 7 days ahead to the extreme precipitation days (top 5%) are examined. The evolutions of the atmospheric circulation patterns and the moisture fluxes are both consistent with the TMEs tracks that contribute more moisture releases to the study regions. The findings imply that atmospheric steering plays an important role in the moisture transport and release, especially for the extreme precipitations. We also find that the association between TMEs moisture release and precipitation is nonlinear. The extreme precipitation is associated with high TMEs moisture release for all of the three study regions.
机译:作为案例研究,提出了三个流域,即长江流域,密西西比河流域和卢瓦尔河流域,以探讨中纬度地区大气环流,水分输出和极端降水之间的关系。首先使用热带水分出口(TME)数据集确定了三个流域热带地区的主要水分源区域。介绍了它们各自水分源的时空特征。然后,将轨迹曲线聚类分析应用于每个盆地TME的峰值活动和汛期期间,从已识别的源区出发的TMEs航迹。我们的结果表明,每个盆地的水分径迹可分为具有不同空间轨迹特征的3或4个簇。我们对这些簇状轨迹的进一步分析表明,来自不同簇的水分释放的贡献与其轨迹特征和行进速度有关。为了理解相关的大气转向的作用,研究了从7天到极端降水天数(最高5%)的地势高度异常和水汽通量异常的垂直积分的日复合值。大气环流模式和水分通量的演变都与TMEs轨迹一致,TMEs轨迹向研究区域贡献了更多的水分。研究结果表明,大气转向在水分输送和释放中起着重要作用,尤其是对于极端降水而言。我们还发现,TMEs水分释放与降水之间的关联是非线性的。在这三个研究区域中,极端降水与高TMEs的水分释放有关。

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