中大學術數位典藏-NCU Institutional Repository:Item 987654321/99810
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 94459/94459 (100%)
造访人次 : 87652507      在线人数 : 310
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/987654321/99810


    题名: An orography-associated extreme rainfall event during TiMREX: Initiation, storm evolution, and maintenance
    作者: 廖宇慶;Xu, Weixin;Zipser, Edward J;Chen, Yi-Leng;Liu, Chuntao;Liou, Yu-Chieng;Lee, Wen-Chau;Jou, Ben Jong-Dao
    贡献者: 地球科學學院大氣科學學系
    关键词: Coastal zone;Cold;Earth, ocean, space;Exact sciences and technology;External geophysics;Extreme weather;Meteorology;Orography;Precipitation;Rain;Rainfall;Upstream;Wind
    日期: 2012-08-01
    上传时间: 2026-04-21 13:36:15 (UTC+8)
    出版者: American Meteorological Society;Boston, MA: American Meteorological Society
    摘要: 摘要: AbstractThis study investigates a long-duration mesoscale system with extremely heavy rainfall over southwest Taiwan during the Terrain-influenced Monsoon Rainfall Experiment (TiMREX). This mesoscale convective system develops offshore and stays quasi-stationary over the upstream ocean and southwest coast of Taiwan. New convection keeps developing upstream offshore but decays or dies after moving into the island, dropping the heaviest rain over the upstream ocean and coastal regions. Warm, moist, unstable conditions and a low-level jet (LLJ) are found only over the upstream ocean, while the island of Taiwan is under the control of a weak cold pool. The LLJ is lifted upward at the boundary between the cold pool and LLJ. Most convective clusters supporting the long-lived rainy mesoscale system are initiated and develop along that boundary. The initiation and maintenance is thought to be a “back-building–quasi-stationary” process. The cold pool forms from previous persistent precipitation with a temperature depression of 2°–4°C in the lowest 500 m, while the high terrain in Taiwan is thought to trap the cold pool from spreading or moving. As a result, the orography of Taiwan is “extended” to the upstream ocean and plays an indirect effect on the long-duration mesoscale system.
    出版者: Boston, MA: American Meteorological Society
    出版日期: 2012-08-01
    出處: Monthly Weather Review, 2012-08, Vol.140 (8), p.2555-2574
    資源來源: EBSCOhost OmniFile Full Text Select
    版權: 2015 INIST-CNRS
    版權: Copyright American Meteorological Society Aug 2012
    識別號: ISSN: 0027-0644
    識別號: ISSN: 1520-0493
    識別號: EISSN: 1520-0493
    識別號: DOI: 10.1175/mwr-d-11-00208.1
    識別號: CODEN: MWREAB
    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.html0KbHTML28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