中大學術數位典藏-NCU Institutional Repository-提供博碩士論文、考古題、期刊論文、研究計畫等下載:Item 987654321/102403
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 94201/94201 (100%)
Visitors : 81481627      Online Users : 3245
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Tips:
  • please add "double quotation mark" for query phrases to get precise results
  • please goto advance search for comprehansive author search
  • Adv. Search
    HomeLoginUploadHelpAboutAdminister Goto mobile version


    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/102403


    Title: Inter-annual and decadal fluctuations of the Kuroshio in East China Sea and connection with surface fluxes of momentum and heat
    Authors: 黃如瑤;Wang, Jia;Oey, Lie-Yauw
    Contributors: 地球科學學院水文與海洋科學研究所
    Keywords: Altimetry;Annual;China;Climate;Coastal;Coastal zone;Coastal zones;Curl (vectors);decadal trend;East China Sea;Fluctuation;Fluctuations;Fluxes;Geophysics;Heat;Heat flux;Heat transfer;interannual variation;kuroshio;Loads (forces);Long-term changes;Marine;Momentum;Northeast;Ocean temperature;Offshore;Satellite altimetry;Satellites;Sea surface;Sea surface temperature;Surface fluxes;surface heat flux;Thermocline;Transport;Wind;Wind stress;Wind stress curl
    Date: 2014-12-16
    Issue Date: 2026-04-23 11:08:05 (UTC+8)
    Publisher: Wiley-Blackwell;Washington: Blackwell Publishing Ltd
    Abstract: 摘要: Despite attempts in the literature to link large‐scale wind to long‐term variations of the Kuroshio in East China Sea (ECS), the driving mechanism(s) are unknown. Here we use satellite altimetry data, wind, surface heat fluxes and sea‐surface temperatures (SST) to explain the low‐frequency fluctuations of Kuroshio path (KP) in ECS. The dominant fluctuations occur northeast of Taiwan. The KP correlates best with the PTO index of Chang and Oey (2012), less with the PDO index and a Kuroshio transport index, and poorly with other climate indices. The forcing are wind stress curl and surface heat flux northeast of Taiwan, which produce a thermocline tilt along the Kuroshio. Shelf's SST warms and cools in response to onshore and offshore KP, but prominent change occurs at a localized coastal zone shoreward of the above dominant KP‐fluctuations. Over the past 2 decades, the KP has shifted onshore, coincident with a coastal warming trend. Key Points Kuroshio fluctuations NE Taiwan are forced by wind and surface heat fluxPTO rather than PDO is a good predictor of Kuroshio fluctuationsCoastal SST warming is closely tied to Kuroshio intrusion
    其他題名: Geophys. Res. Lett
    出版者: Washington: Blackwell Publishing Ltd
    出版日期: 2014-12-16
    出處: Geophysical research letters, 2014-12, Vol.41 (23), p.8538-8546
    資源來源: Wiley Online Library
    版權: 2014. American Geophysical Union. All Rights Reserved.
    版權: 2015. American Geophysical Union. All Rights Reserved.
    版權: Copyright Blackwell Publishing Ltd. Dec 2014
    識別號: ISSN: 0094-8276
    識別號: ISSN: 1944-8007
    識別號: EISSN: 1944-8007
    識別號: DOI: 10.1002/2014GL062118
    Appears in Collections:[Graduate Institute of Hydrological and Oceanic Sciences] journal & Dissertation

    Files in This Item:

    File Description SizeFormat
    index.html0KbHTML13View/Open


    All items in NCUIR are protected by copyright, with all rights reserved.

    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