中大學術數位典藏-NCU Institutional Repository:Item 987654321/100614
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 94459/94459 (100%)
造访人次 : 87652283      在线人数 : 239
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜寻范围 查询小技巧:
  • 您可在西文检索词汇前后加上"双引号",以获取较精准的检索结果
  • 若欲以作者姓名搜寻,建议至进阶搜寻限定作者字段,可获得较完整数据
  • 进阶搜寻


    jsp.display-item.identifier=請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/100614


    题名: A modeling study on the effects of MJO and equatorial Rossby waves on tropical cyclone genesis over the western North Pacific in June 2004
    作者: 林沛練;Ching, Lin;Sui, Chung-Hsiung;Yang, Ming-Jen;Lin, Pay-Liam
    贡献者: 地球科學學院大氣科學學系
    关键词: Marine;MJO;Numerical simulation;Rossby wave;Tropical cyclogenesis;WRF
    日期: 2015-12-01
    上传时间: 2026-04-21 14:08:45 (UTC+8)
    出版者: Elsevier BV;Elsevier B.V
    摘要: 摘要: •The impacts of multi-scale tropical waves on tropical cyclogenesis are explored.•A novel method of using filtering to remove the waves in the WRF model is employed.•Removal of specific tropical wave in the sensitivity experiment is reasonable.•The numerical approach helps us to investigate the contribution of tropical waves. This study investigates the influence of the Madden Julian oscillations (MJO) and equatorial Rossby (ER) waves on tropical cyclone (TC) formation in western Pacific during June 2004 through one control and three wave experiments for each of the five TCs. The control experiment reasonably simulates the formation of five TCs. In the corresponding wave experiments, the MJO, ER waves, and both the MJO and ER waves are removed, from the initial fields and lateral boundary conditions, respectively. The differences of simulated TC intensity between the control and corresponding wave experiments provide a quantitative assessment of the relative contribution of each wave to TC formation. In the wave experiments with the MJO removed, three of the five TCs are weakened, and the remaining two (TC A and B) grow stronger due to an altered background flow that steered the TCs into more favorable oceanic regions. For the wave experiments with ER waves removed, three of the five simulated TCs become weaker (TC A, C, and E). TC D develops into a tropical storm because of a dominant influence from active synoptic-scale disturbance. The results indicate that both the MJO and ER waves have an important modulating effect on TC formation. In addition to the influence from the MJO, ER and synoptic-scale waves, local processes may dominate in TC formation; for the example of TC B, none of the waves positively influence the formation in significant ways. The present modeling approach provides a quantitative assessment of the relative contribution of tropical wave disturbances to TC formation.
    出版者: Elsevier B.V
    出版日期: 2015-12
    出處: Dynamics of atmospheres and oceans, 2015-12, Vol.72, p.70-87
    資源來源: Elsevier ScienceDirect Journals Complete
    版權: 2015 Elsevier B.V.
    識別號: ISSN: 0377-0265
    識別號: EISSN: 1872-6879
    識別號: DOI: 10.1016/j.dynatmoce.2015.10.002
    显示于类别:[大氣科學學系] 期刊論文

    文件中的档案:

    档案 描述 大小格式浏览次数
    index.html0KbHTML27检视/开启


    在NCUIR中所有的数据项都受到原著作权保护.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明