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Impacts of four types of ENSO events on tropical cyclones making landfall over mainland china based on three best-track datasets

机译:基于三个最佳轨道数据集,四种ENsO事件对在中国大陆登陆的热带气旋的影响

摘要

Impacts of El Nio Modoki (ENM), La Nia Modoki (LNM), canonical El Nio (CEN) and canonical La Nia (CLN) on tropical cyclones (TCs) that made landfall over mainland China during 1951-2011 are analysed using best-track data from China, the USA and Japan. Relative to cold phase years (LNM and CLN), landfalling TCs in warm years (ENM and CEN) have a farther east genesis location, as well as longer track lengths and durations, both in total and before landfall. ENM demonstrates the highest landfall frequency, most northerly mean landfall position, and shortest after-landfall sustainability (track length and duration), which indicate a more frequent and extensive coverage of mainland China by TCs, but with shorter after-landfall influence. CEN has low landfall frequency and the most southerly mean landfall location. LNM has the most westerly genesis location, being significantly farther west than the 1951-2011 average and leading to short mean track lengths and durations both in total or before landfall, all of which are significantly shorter than the 1951-2011 average. Variations in the low-level wind anomaly, vertical wind shear, mid-level relative humidity, steering flow, the monsoon trough and the western Pacific subtropical high (WPSH) can to some extent account for the features of frequency, location, track length and duration of landfalling TCs. Since ENSO Modoki is expected to become more frequent in the near future, the results for ENSO Modoki presented in this paper are of particular significance.
机译:厄尔尼诺·莫迪基(ENM),拉尼娅·莫迪基(LNM),规范的尼奥(CEN)和规范的拉尼娅(CLN)对热带气旋(TCs)在1951-2011年期间登陆中国大陆的影响进行了分析,跟踪来自中国,美国和日本的数据。相对于寒冷时期(LNM和CLN),温暖年份(ENM和CEN)的降落TCs的东部成因位置更远,并且在总的和登陆前的轨道长度和持续时间更长。 ENM展示了最高的登陆频率,最北偏北的平均登陆位置以及最短的登陆后可持续性(航迹长度和持续时间),这表明TC覆盖中国大陆的频率更高,覆盖面更广,但登陆后的影响力更短。 CEN的登陆频率较低,并且平均登陆位置偏南。 LNM的发生位置最西风,比1951-2011年的平均值明显偏西,导致总体或登陆前的平均航迹长度和持续时间较短,所有这些均明显短于1951-2011年的平均值。低层风异常,垂直风切变,中层相对湿度,转向流,季风槽和西太平洋副热带高压(WPSH)的变化在一定程度上可以解释频率,位置,轨道长度和降落TC的持续时间。由于预计ENSO Modoki在不久的将来会越来越频繁,因此本文提出的ENSO Modoki的结果具有特别的意义。

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    Zhang H; Guan YP;

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  • 年度 2014
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