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    Observations of the Flow of Abyssal Water through the Samoa Passage

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 008::page 2273
    Author:
    Freeland, Howard
    DOI: 10.1175/1520-0485(2001)031<2273:OOTFOA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: During the fall of 1994 a conductivity?temperature?depth/hydrographic survey was carried out as part of the World Ocean Circulation Experiment one-time survey, Line P15N. The survey included standard water properties required by WOCE. Line P15N extended southward from the Aleutian Islands along 165°W into the vicinity of the Samoa Passage. The line was adjusted to follow the axis of the passage, and time was found to complete a cross-section survey across the passage. This paper will present geostrophic computations of flow velocities through the gap, including transport estimates, and will present longitudinal plots of properties. The longitudinal plots show evidence of hydraulic control at the sill in the Samoa Passage. A best estimate of northward transport of water colder than 1.2°C (potential temperature) is determined to be 8.4 Sv.
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      Observations of the Flow of Abyssal Water through the Samoa Passage

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4166730
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    contributor authorFreeland, Howard
    date accessioned2017-06-09T14:54:43Z
    date available2017-06-09T14:54:43Z
    date copyright2001/08/01
    date issued2001
    identifier issn0022-3670
    identifier otherams-29497.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166730
    description abstractDuring the fall of 1994 a conductivity?temperature?depth/hydrographic survey was carried out as part of the World Ocean Circulation Experiment one-time survey, Line P15N. The survey included standard water properties required by WOCE. Line P15N extended southward from the Aleutian Islands along 165°W into the vicinity of the Samoa Passage. The line was adjusted to follow the axis of the passage, and time was found to complete a cross-section survey across the passage. This paper will present geostrophic computations of flow velocities through the gap, including transport estimates, and will present longitudinal plots of properties. The longitudinal plots show evidence of hydraulic control at the sill in the Samoa Passage. A best estimate of northward transport of water colder than 1.2°C (potential temperature) is determined to be 8.4 Sv.
    publisherAmerican Meteorological Society
    titleObservations of the Flow of Abyssal Water through the Samoa Passage
    typeJournal Paper
    journal volume31
    journal issue8
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2001)031<2273:OOTFOA>2.0.CO;2
    journal fristpage2273
    journal lastpage2279
    treeJournal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 008
    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
    yabeshDSpacePersian