YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Bulletin of the American Meteorological Society
    • View Item
    •   YE&T Library
    • AMS
    • Bulletin of the American Meteorological Society
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    The Definition of El Niño

    Source: Bulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 012::page 2771
    Author:
    Trenberth, Kevin E.
    DOI: 10.1175/1520-0477(1997)078<2771:TDOENO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A review is given of the meaning of the term "El Niño" and how it has changed in time, so there is no universal single definition. This needs to be recognized for scientific uses, and precision can only be achieved if the particular definition is identified in each use to reduce the possibility of misunderstanding. For quantitative purposes, possible definitions are explored that match the El Niños identified historically after 1950, and it is suggested that an El Niño can be said to occur if 5-month running means of sea surface temperature (SST) anomalies in the Niño 3.4 region (5°N?5°S, 120°?170°W) exceed 0.4°C for 6 months or more. With this definition, El Niños occur 31% of the time and La Niñas (with an equivalent definition) occur 23% of the time. The histogram of Niño 3.4 SST anomalies reveals a bimodal character. An advantage of such a definition is that it allows the beginning, end, duration, and magnitude of each event to be quantified. Most El Niños begin in the northern spring or perhaps summer and peak from November to January in sea surface temperatures.
    • Download: (130.9Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Statistics

      The Definition of El Niño

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4161481
    Collections
    • Bulletin of the American Meteorological Society

    Show full item record

    contributor authorTrenberth, Kevin E.
    date accessioned2017-06-09T14:42:02Z
    date available2017-06-09T14:42:02Z
    date copyright1997/12/01
    date issued1997
    identifier issn0003-0007
    identifier otherams-24772.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161481
    description abstractA review is given of the meaning of the term "El Niño" and how it has changed in time, so there is no universal single definition. This needs to be recognized for scientific uses, and precision can only be achieved if the particular definition is identified in each use to reduce the possibility of misunderstanding. For quantitative purposes, possible definitions are explored that match the El Niños identified historically after 1950, and it is suggested that an El Niño can be said to occur if 5-month running means of sea surface temperature (SST) anomalies in the Niño 3.4 region (5°N?5°S, 120°?170°W) exceed 0.4°C for 6 months or more. With this definition, El Niños occur 31% of the time and La Niñas (with an equivalent definition) occur 23% of the time. The histogram of Niño 3.4 SST anomalies reveals a bimodal character. An advantage of such a definition is that it allows the beginning, end, duration, and magnitude of each event to be quantified. Most El Niños begin in the northern spring or perhaps summer and peak from November to January in sea surface temperatures.
    publisherAmerican Meteorological Society
    titleThe Definition of El Niño
    typeJournal Paper
    journal volume78
    journal issue12
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1997)078<2771:TDOENO>2.0.CO;2
    journal fristpage2771
    journal lastpage2777
    treeBulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 012
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian