首页> 外文期刊>Acta Meteorologica Sinica >LOW FREQUENCY OSCILLATION IN EAST ASIA DURING THE 1991 EXCESSIVELY HEAVY RAIN OVER THE CHANGJIANG-HUAIHE RIVER BASIN
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LOW FREQUENCY OSCILLATION IN EAST ASIA DURING THE 1991 EXCESSIVELY HEAVY RAIN OVER THE CHANGJIANG-HUAIHE RIVER BASIN

机译:1991年长江-淮河流域东亚暴雨期间的东亚低频振荡

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摘要

The activity of low frequency oscillation (LFO) widely exists in East Asia during the period of 1991 excessively heavy rain over the Changjiang-Huaihe River Basin (Jianghuai). Both the rainfall amount of Jianghuai and the atmosphere from subtropical area to mid-high latitudes have the dominant period of 10- 20 d, while the atmospheres in tropical area and high latitudes have the dominant period of 30 - 60 d. Compared with normal Meiyu season, the anomaly of the 1991 Meiyu process may be reflected in the following two low frequency synoptic events: (a) The Meiyu process onsets extremely early (in the second dekad of May, which is nearly one month earlier than in normal Meiyu) and is immediately followed by the first episode of heavy rain. (b) In the first dekad of July, there occurs the heaviest episode of rainfall of the whole Meiyu season, and it is even the heaviest rainfall for the recent 30 years in China. For these two periods, corresponding to the adjustment of large-scale situation from "double blocking high" to "bipolar blocking high", the propagation direction of LFO in East Asia has a distinct seasonal variation, from eastwardorth ward propagation (passing through Jianghuai) during the first episode to west ward/southward propagation during the third episode. Oscillations of different frequency bands are superposed in phase. The LFO activity of the cold and warm/moist airs over Jianghuai can be strengthened through those LFO propagation processes in East Asia, although they may have different directions in three episodes. Particularly, the eastward (westward) propagation in low latitudes makes the southwest (southeast) airflow transport intensively the low frequency warm/moist air to the south of Jianghuai from the Indian Ocean (tropical West Pacific Ocean) in the first (third) episode. Such warm/moist airs meet and interact with the cold air which vigorously invades Jianghuai persistently, and finally three episodes of heavy rain occur in mode of LFO.
机译:1991年,长江-淮河流域(江淮)暴雨过多,低频振荡(LFO)活动在东亚广泛存在。江淮的降水量和亚热带地区至中高纬度地区的大气的主导时期均为10〜20 d,而热带地区和高纬度地区的大气的主导时期为30〜60 d。与正常的梅雨季节相比,1991年梅雨过程的异常可能反映在以下两个低频天气事件中:(a)梅雨过程开始得非常早(5月的第二个十月,比5月的近十个月早了一个月)。正常的梅雨),然后是第一场大雨。 (b)在7月的第一个十年,发生了整个梅雨季节的最大降雨,甚至是近30年来中国最大的降雨。在这两个时期,对应于从“双阻塞高”向“双极阻塞高”的大范围调整,东亚地区低频振荡的传播方向从东向/北向传播(通过江淮)在第一集中向西向南传播。不同频带的振荡同相叠加。通过在东亚的LFO传播过程,可以增强江淮上冷,暖/湿空气的LFO活动,尽管它们在三个情节中可能有不同的方向。特别是,低纬度向东(向西)传播使西南(东南)气流在第一(第三)次集中从印度洋(热带西太平洋)向江淮以南的低频温暖/潮湿空气的集中输送。这些温暖/潮湿的空气与冷空气相遇并相互作用,而冷空气不断地侵入江淮,最后以LFO模式发生了三场大雨。

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