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    Diabatic Upwelling in the Tropical Pacific: Seasonal and Subseasonal Variability

    Source: Journal of Physical Oceanography:;2022:;volume( 052 ):;issue: 011::page 2657
    Author:
    Anna-Lena Deppenmeier
    ,
    Frank O. Bryan
    ,
    William S. Kessler
    ,
    LuAnne Thompson
    DOI: 10.1175/JPO-D-21-0316.1
    Publisher: American Meteorological Society
    Abstract: The equatorial Pacific zonal circulation is composed of westward surface currents, the eastward equatorial undercurrent (EUC) along the thermocline, and upwelling in the eastern cold tongue. Part of this upwelling arises from water flowing along isotherms sloping up to the east, but it also includes water mass transformation and consequent diabatic (cross-isothermal) flow (
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      Diabatic Upwelling in the Tropical Pacific: Seasonal and Subseasonal Variability

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4289892
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    contributor authorAnna-Lena Deppenmeier
    contributor authorFrank O. Bryan
    contributor authorWilliam S. Kessler
    contributor authorLuAnne Thompson
    date accessioned2023-04-12T18:34:06Z
    date available2023-04-12T18:34:06Z
    date copyright2022/10/21
    date issued2022
    identifier otherJPO-D-21-0316.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289892
    description abstractThe equatorial Pacific zonal circulation is composed of westward surface currents, the eastward equatorial undercurrent (EUC) along the thermocline, and upwelling in the eastern cold tongue. Part of this upwelling arises from water flowing along isotherms sloping up to the east, but it also includes water mass transformation and consequent diabatic (cross-isothermal) flow (
    publisherAmerican Meteorological Society
    titleDiabatic Upwelling in the Tropical Pacific: Seasonal and Subseasonal Variability
    typeJournal Paper
    journal volume52
    journal issue11
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-21-0316.1
    journal fristpage2657
    journal lastpage2668
    page2657–2668
    treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 011
    contenttypeFulltext
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