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    Numerical Study of the Seasonal Variations of the Subtropical Front and the Subtropical Countercurrent

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005::page 919
    Author:
    Takeuchi, Kensuke
    DOI: 10.1175/1520-0485(1986)016<0919:NSOTSV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Response of the Subtropical Countercurrent and the Subtropical Front in the North Pacific Ocean to seasonally changing wind stress and thermal condition are examined using the same idealized numerical model that the author used in 1984 for steady state modeling of the Subtropical Countercurrent and the Subtropical Front. The model reproduces the main features of the observed seasonal variations reasonably well, especially that the Subtropical Countercurrent is strong in spring and weak in fall. It is also shown that the seasonal variation of wind stress and thermal condition intensifies the annual mean strength of the Subtropical Countercurrent. The relative importance of the seasonal variations of wind stress and thermal condition is examined using models in which only one of these changes and the other is fixed. The results indicate that the seasonal variation of the Subtropical Countercurrent is mainly due to the seasonal change of wind stress, while the seasonal change of thermal condition is mostly responsible for the intensification of the annual mean of the Subtropical Countercurrent and the Subtropical Front.
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      Numerical Study of the Seasonal Variations of the Subtropical Front and the Subtropical Countercurrent

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163962
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    contributor authorTakeuchi, Kensuke
    date accessioned2017-06-09T14:47:54Z
    date available2017-06-09T14:47:54Z
    date copyright1986/05/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-27004.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163962
    description abstractResponse of the Subtropical Countercurrent and the Subtropical Front in the North Pacific Ocean to seasonally changing wind stress and thermal condition are examined using the same idealized numerical model that the author used in 1984 for steady state modeling of the Subtropical Countercurrent and the Subtropical Front. The model reproduces the main features of the observed seasonal variations reasonably well, especially that the Subtropical Countercurrent is strong in spring and weak in fall. It is also shown that the seasonal variation of wind stress and thermal condition intensifies the annual mean strength of the Subtropical Countercurrent. The relative importance of the seasonal variations of wind stress and thermal condition is examined using models in which only one of these changes and the other is fixed. The results indicate that the seasonal variation of the Subtropical Countercurrent is mainly due to the seasonal change of wind stress, while the seasonal change of thermal condition is mostly responsible for the intensification of the annual mean of the Subtropical Countercurrent and the Subtropical Front.
    publisherAmerican Meteorological Society
    titleNumerical Study of the Seasonal Variations of the Subtropical Front and the Subtropical Countercurrent
    typeJournal Paper
    journal volume16
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<0919:NSOTSV>2.0.CO;2
    journal fristpage919
    journal lastpage926
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005
    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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