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    On the deep general circulation in the western North Atlantic

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    WHOI-78-3.pdf (21.75Mb)
    Date
    1978-04
    Author
    Schmitz, William J.  Concept link
    Metadata
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    Citable URI
    https://hdl.handle.net/1912/10589
    DOI
    10.1575/1912/10589
    Keyword
    Ocean circulation
    Abstract
    Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the vicinity of a recently hypothesized (Worthington, in press) horizontally restricted subtropical gyre in the deep western North Atlantic. The Reynolds stresses associated with low frequency fluctuations may play a significant role in the dynamics of this deep mean flow, possibly inducing a significant downstream increase in transport of the Gulf Stream, perhaps driving the deep gyre.
    Description
    Also published as: Journal of Marine Research, Volume 35, 1977, pp. 21-28
    Collections
    • Physical Oceanography (PO)
    • WHOI Technical Reports
    Suggested Citation
    Schmitz, W. J. (1978). On the deep general circulation in the western North Atlantic. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/10589
     

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