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    Representation of the Equatorial Undercurrent in CMIP5 Models

    Source: Journal of Physical Oceanography:;2020:;volume( 50 ):;issue: 010::page 2997
    Author:
    Kuntz, Lauren B.;Schrag, Daniel P.
    DOI: 10.1175/JPO-D-20-0007.1
    Publisher: American Meteorological Society
    Abstract: The Equatorial Undercurrent (EUC) is a vital component of tropical Pacific circulation, helping to modulate the state of the equatorial Pacific Ocean. Here we compare the representation of the EUC in models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) with observations of the undercurrent. We find that the CMIP5 models consistently underestimate both the magnitude and variability of the EUC. Insufficient resolution as well as diffusivity parameterizations both contribute to a representation of the EUC that is too weak and too diffuse. Given the strong influence of the EUC on the evolution of tropical Pacific sea surface temperatures, model deficiencies in the EUC contribute to shortcomings in capturing ENSO dynamics and Pacific decadal variability. Further evaluation of the impact of EUC simulation on the climatology and variability in the tropical Pacific is necessary.
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      Representation of the Equatorial Undercurrent in CMIP5 Models

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    contributor authorKuntz, Lauren B.;Schrag, Daniel P.
    date accessioned2022-01-30T18:05:07Z
    date available2022-01-30T18:05:07Z
    date copyright10/7/2020 12:00:00 AM
    date issued2020
    identifier issn0022-3670
    identifier otherjpod200007.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4264466
    description abstractThe Equatorial Undercurrent (EUC) is a vital component of tropical Pacific circulation, helping to modulate the state of the equatorial Pacific Ocean. Here we compare the representation of the EUC in models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) with observations of the undercurrent. We find that the CMIP5 models consistently underestimate both the magnitude and variability of the EUC. Insufficient resolution as well as diffusivity parameterizations both contribute to a representation of the EUC that is too weak and too diffuse. Given the strong influence of the EUC on the evolution of tropical Pacific sea surface temperatures, model deficiencies in the EUC contribute to shortcomings in capturing ENSO dynamics and Pacific decadal variability. Further evaluation of the impact of EUC simulation on the climatology and variability in the tropical Pacific is necessary.
    publisherAmerican Meteorological Society
    titleRepresentation of the Equatorial Undercurrent in CMIP5 Models
    typeJournal Paper
    journal volume50
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-20-0007.1
    journal fristpage2997
    journal lastpage3007
    treeJournal of Physical Oceanography:;2020:;volume( 50 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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