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    Interannual Variations of North Pacific Subtropical Mode Water in the 137°E Section

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 005::page 1012
    Author:
    Suga, Toshio
    ,
    Hanawa, Kimio
    DOI: 10.1175/1520-0485(1995)025<1012:IVONPS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Examination of interannual variations of North Pacific subtropical mode water (STMW) in the 137°E repeat hydrographic section by Suga et al. is extended to seek a relation between changes in STMW renewal and the wintertime cooling. Time series of isopycnal potential vorticity (PV) and apparent oxygen utilization (AOU) demonstrate substantial interannual variations of STMW. It is suggested that the interannual variations are closely related to the changes both in the Kuroshio recirculation system and in the formation rate. For the non-large-meander period of the Kuroshio, during which renewed STMW is advected vigorously from east of the section, the monsoon index as an indicator of cooling in a given winter, and PV and AOU at an STMW isopycnal surface in the following summer show significant correlation, indicating a strong relation between the wintertime cooling and the STMW formation.
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      Interannual Variations of North Pacific Subtropical Mode Water in the 137°E Section

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4165415
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    contributor authorSuga, Toshio
    contributor authorHanawa, Kimio
    date accessioned2017-06-09T14:51:27Z
    date available2017-06-09T14:51:27Z
    date copyright1995/05/01
    date issued1995
    identifier issn0022-3670
    identifier otherams-28312.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165415
    description abstractExamination of interannual variations of North Pacific subtropical mode water (STMW) in the 137°E repeat hydrographic section by Suga et al. is extended to seek a relation between changes in STMW renewal and the wintertime cooling. Time series of isopycnal potential vorticity (PV) and apparent oxygen utilization (AOU) demonstrate substantial interannual variations of STMW. It is suggested that the interannual variations are closely related to the changes both in the Kuroshio recirculation system and in the formation rate. For the non-large-meander period of the Kuroshio, during which renewed STMW is advected vigorously from east of the section, the monsoon index as an indicator of cooling in a given winter, and PV and AOU at an STMW isopycnal surface in the following summer show significant correlation, indicating a strong relation between the wintertime cooling and the STMW formation.
    publisherAmerican Meteorological Society
    titleInterannual Variations of North Pacific Subtropical Mode Water in the 137°E Section
    typeJournal Paper
    journal volume25
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1995)025<1012:IVONPS>2.0.CO;2
    journal fristpage1012
    journal lastpage1017
    treeJournal of Physical Oceanography:;1995:;Volume( 025 ):;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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