University of Taipei:Item 987654321/2570
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 2471/17084 (14%)
Visitors : 3183971      Online Users : 1076
RC Version 6.0 © 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: http://utaipeir.lib.utaipei.edu.tw/dspace/handle/987654321/2570


    Title: Temporal and spatial characteristics of positive and negative Indian Ocean dipole with and without ENSO
    Authors: Chi-Cherng Hong
    Mong-Ming Lu
    Masao Kanamitsu
    洪志誠
    Contributors: 臺北市立教育大學自然科學系
    Date: 2008
    Issue Date: 2009-07-27 13:50:37 (UTC+8)
    Abstract: The differences in the temporal evolution and spatial characteristics of the Indian Ocean Dipole (IOD) between positive and negative events with and without ENSO have been investigated using observations for the period 1948–2002. To document such differences is particularly important for climate forecasts over far east Asia, since distinctly different monsoon activities over China, Korea, and Japan for different types of IOD are found in the composite maps of precipitation anomalies. The composite map of SST and wind during various stages of IOD and the ocean mixed layer heat budget showed that the IOD with and without ENSO has a large difference in its temporal evolutions and their triggering mechanisms. In both negative and positive IOD events without ENSO, the wind anomaly in the eastern Indian Ocean seems to be responsible for the formation of sea surface temperature anomalies, while the anomaly in the western Indian Ocean seems to be the oceanic dynamical response to the anomaly in the east. During the ENSO years, the temporal and spatial contrast of the asymmetry of the IOD evolution is smaller, and the SST anomaly is driven by the anomalies in incoming radiation due to changes in cloudiness caused by the ENSO associated anomalous atmospheric circulations and not by the local wind anomalies.
    Relation: J. Geophys, p. 113
    Appears in Collections:[Department of Applied Physics and Chemistry] Periodical Articles

    Files in This Item:

    There are no files associated with this item.



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


    如有問題歡迎與系統管理員聯繫
    02-23113040轉2132
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback