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dc.contributor.authorSantoso, Agus
dc.contributor.authorCai, Wenju
dc.contributor.authorCollins, Matthew
dc.contributor.authorMcPhaden, Michael J.
dc.contributor.authorJin, Fei-Fei
dc.contributor.authorGuilyardi, Eric
dc.contributor.authorVecchi, Gabriel
dc.contributor.authorDommenget, Dietmar
dc.contributor.authorWang, Guojian
dc.date.accessioned2016-02-12T10:01:19Z
dc.date.issued2015-11
dc.description.abstractIn boreal spring of 2014, the tropical Pacific was primed for an El Niño, when most forecast agencies such as the National Oceanic and Atmospheric Administration (NOAA) and the Australian Bureau of Meteorology elevated their El Niño probability to more than 60%. A remarkable increase in warm water volume with a series of westerly wind bursts in boreal spring alerted the El Niño Southern Oscillation (ENSO) experts to the possibility of a strong event. The mean climate, upon which ENSO evolved, varied on multi-decadal time scales, manifesting itself as a global-scale phenomenon in what is commonly known as the IPO or PDO.en_GB
dc.description.sponsorshipCSIROen_GB
dc.description.sponsorshipAustralian Research Council (ARC) Centre of Excellence for Climate System Scienceen_GB
dc.identifier.citationVol. 96 (11), pp. 1969 - 1972en_GB
dc.identifier.doi10.1175/BAMS-D-15-00141.1
dc.identifier.urihttp://hdl.handle.net/10871/19759
dc.language.isoenen_GB
dc.publisherAmerican Meteorological Societyen_GB
dc.rights.embargoreasonPublisher policyen_GB
dc.rights© Copyright 2015 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyrights@ametsoc.org.en_GB
dc.titleEnso extremes and diversity: Dynamics, teleconnections, and impactsen_GB
dc.typeArticleen_GB
dc.identifier.issn0003-0007
dc.identifier.journalBulletin of the American Meteorological Societyen_GB


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