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    Modeling 18° Water Variability 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 006:;page 1059
    Author(s): Marsh, Robert; New, Adrian L.
    Publisher: American Meteorological Society
    Abstract: Variability of 18° Water formation is investigated with an isopycnic-coordinate model of the North Atlantic. A 30-year spinup integration is used as a ?control? experiment in which the upper water column in the Sargasso ...
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    An Intercomparison of a Bryan–Cox-Type Ocean Model and an Isopycnic Ocean Model. Part I: The Subpolar Gyre and High-Latitude Processes 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 008:;page 1495
    Author(s): Roberts, Malcolm J.; Wood, Richard A.; Marsh, Robert; New, Adrian L.
    Publisher: American Meteorological Society
    Abstract: This paper describes a model intercomparison between a Bryan-Cox-type ocean model and an isopycnic-coordinate ocean model. The two models are integrated for 30 years on a domain of the North Atlantic stretching from 20°S ...
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    An Intercomparison of a Bryan-Cox-Type Ocean Model and an Isopycnic Ocean Model. Part II: The Subtropical Gyre and Meridional Heat Transport 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 008:;page 1528
    Author(s): Marsh, Robert; New, Adrian L.; Roberts, Malcolm J.; Wood, Richard A.
    Publisher: American Meteorological Society
    Abstract: In a companion paper, two ocean general circulation models were implemented in order to simulate and intercompare the main features of the North Atlantic circulation: the Atlantic Isopycnic Model (AIM) and the Hadley Centre ...
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    Water Mass Transformation in the Southern Ocean of a Global Isopycnal Coordinate GCM 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 005:;page 1013
    Author(s): Marsh, Robert; Nurser, A. J. George; Megann, Alex P.; New, Adrian L.
    Publisher: American Meteorological Society
    Abstract: A global isopycnal coordinate GCM is used to investigate the processes that drive the meridional circulation, transformation, and interocean exchange of water masses in the Southern Ocean. The noneddy-resolving model (mesh ...
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