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    2015 Bernhard Haurwitz Memorial Lecture: Model Diagnosis of El Niño Teleconnections to the Global Atmosphere–Ocean System

    Source: Bulletin of the American Meteorological Society:;2015:;volume( 097 ):;issue: 006::page 981
    Author:
    Lau, Ngar-Cheung
    DOI: 10.1175/BAMS-D-15-00220.1
    Publisher: American Meteorological Society
    Abstract: he El Niño?Southern Oscillation (ENSO) phenomenon is one of the most prominent modes of atmospheric and oceanic variability on interannual and interdecadal time scales. The essential ENSO signals originate from the tropical Pacific (TP). However, the impacts of ENSO are felt in many other parts of the world. Major ENSO events are accompanied by notable changes in the extratropical atmospheric circulation in both hemispheres, various monsoon systems located beyond the TP, global air temperature and precipitation patterns, and the sea surface temperature (SST) distribution throughout the World Ocean. During the past several decades, this author has participated in a sustained effort to study the processes contributing to these ?teleconnections? between ENSO forcing in the TP and variations in the atmosphere?ocean system elsewhere. These investigations are based on a large suite of experiments with several generations of general circulation models (GCMs) at the Geophysical Fluid Dynamics Laboratory (GFDL). These experiments are specifically designed to reveal various facets of the teleconnections with ENSO. In this lecture, a summary is given of the principal findings of this series of model studies. An account is given of the train of thought underpinning the sequence of experiments described herein, so as to illustrate how certain experimental setups have been motivated by the problem or hypothesis at hand.
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      2015 Bernhard Haurwitz Memorial Lecture: Model Diagnosis of El Niño Teleconnections to the Global Atmosphere–Ocean System

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4215924
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    contributor authorLau, Ngar-Cheung
    date accessioned2017-06-09T16:46:12Z
    date available2017-06-09T16:46:12Z
    date copyright2016/06/01
    date issued2015
    identifier issn0003-0007
    identifier otherams-73773.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215924
    description abstracthe El Niño?Southern Oscillation (ENSO) phenomenon is one of the most prominent modes of atmospheric and oceanic variability on interannual and interdecadal time scales. The essential ENSO signals originate from the tropical Pacific (TP). However, the impacts of ENSO are felt in many other parts of the world. Major ENSO events are accompanied by notable changes in the extratropical atmospheric circulation in both hemispheres, various monsoon systems located beyond the TP, global air temperature and precipitation patterns, and the sea surface temperature (SST) distribution throughout the World Ocean. During the past several decades, this author has participated in a sustained effort to study the processes contributing to these ?teleconnections? between ENSO forcing in the TP and variations in the atmosphere?ocean system elsewhere. These investigations are based on a large suite of experiments with several generations of general circulation models (GCMs) at the Geophysical Fluid Dynamics Laboratory (GFDL). These experiments are specifically designed to reveal various facets of the teleconnections with ENSO. In this lecture, a summary is given of the principal findings of this series of model studies. An account is given of the train of thought underpinning the sequence of experiments described herein, so as to illustrate how certain experimental setups have been motivated by the problem or hypothesis at hand.
    publisherAmerican Meteorological Society
    title2015 Bernhard Haurwitz Memorial Lecture: Model Diagnosis of El Niño Teleconnections to the Global Atmosphere–Ocean System
    typeJournal Paper
    journal volume97
    journal issue6
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-15-00220.1
    journal fristpage981
    journal lastpage988
    treeBulletin of the American Meteorological Society:;2015:;volume( 097 ):;issue: 006
    contenttypeFulltext
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