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Trend of precipitation in China and its linkage with El Nino- Southern Oscillation (ENSO)

机译:中国的降水趋势及其与厄尔尼诺-南方涛动的联系

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Plausible long-term trend of precipitation in China is detected by using Mann-Kendall test. The results show that the precipitation mainly increased in the western part of China and mainly decreased in the eastern part of China during the past five decades. The teleconnection between precipitation and El Nino-Southern Oscillation (ENSO) is investigated by using the Student's t-test and 62 stations were found to show a significant difference in precipitation between El Nino and La Nina episodes. Most of these stations are concentrated in the Yellow River basin and Shandong Province. It indicates that the impact of ENSO on precipitation in these regions is greater than that in other regions of China. Average precipitation during El Nino and La Nina episodes, and the entire periods are compared. The results show that La Nina generally coincides with wetter years and El Nino coincides with drier (wetter) years north (south) of the Yangtze River.
机译:利用Mann-Kendall检验可以发现中国降水的长期趋势。结果表明,过去五十年来,降水主要在中国西部增加,主要在中国东部减少。使用学生t检验对降水与厄尔尼诺-南方涛动(ENSO)之间的遥相关进行了研究,发现62个台站显示出厄尔尼诺和拉尼娜事件之间的降水存在显着差异。这些站大多数集中在黄河流域和山东省。这表明ENSO对这些地区降水的影响大于中国其他地区。比较了厄尔尼诺(El Nino)和拉尼娜(La Nina)事件以及整个时期的平均降水量。结果表明,拉尼娜通常与较湿润的年份相吻合,而厄尔尼诺现象与长江以北(南部)的较干燥(较湿)年相吻合。

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