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    Transient Gulf Stream Meandering. Part II: Analysis via a Quasi-Geostrophic Time-Dependent Model 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 002:;page 256
    Author(s): Luyten, J. R.; Robinson, A. R.
    Publisher: American Meteorological Society
    Abstract: Simultaneous path and bottom velocity measurements made during the Transient Meander Experiment, reported in Part I, are analyzed in terms of a quasi-geostrophic thin jet model of the meandering Gulf Stream. The theory ...
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    On the Dynamics of the Coupled Mixed Layer-Thermocline System and the Determination of the Oceanic Surface Density 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 007:;page 1159
    Author(s): Pedlosky, Joseph; Smith, Wendy; Luyten, J. R.
    Publisher: American Meteorological Society
    Abstract: A simple model of the oceanic mixed layer is coupled to a model of the ventilated thermocline. The model allows a combination of advection and surface heating to determine the position of the outcrop lines of the isopycnals. ...
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    The Ventilated Thermocline 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 002:;page 292
    Author(s): Luyten, J. R.; Pedlosky, J.; Stommel, H.
    Publisher: American Meteorological Society
    Abstract: A simple theoretical model for the oceanic thermocline and the associated field of current is presented. The model consists of a finite but arbitarily large number of inviscid, homogeneous fluid layers each with a different ...
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    Transient Gulf Stream Meandering. Part I: An Observational Experiment 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 002:;page 237
    Author(s): Robinson, A. R.; Luyten, J. R.; Fuglister, F. C.
    Publisher: American Meteorological Society
    Abstract: The results from an observational experiment on the mesoscale space-time variability of the Gulf Stream are reported. Various techniques, including aerial surveys, ship trackings of the 15C isotherm at 200 m, drogues and ...
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