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    Wind-Forced Seasonal Exchange between Marginal Seas and the Open Ocean 

    Source: Journal of Physical Oceanography:;2023:;volume( 053 ):;issue: 003:;page 763
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
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    Cooling Spirals and Recirculation in the Subtropical Gyre 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 005:;page 564
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: The influence of cooling in a western boundary current on the recirculation of parcels in the subtropical gyre and their eventual transfer into the subpolar gyre is investigated. It is shown that heat loss to the atmosphere ...
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    Rossby Wave Radiation in the Cape Verde Frontal Zone 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 007:;page 796
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: Radiating baroclinic Rossby waves excited through instability of the Cape Verde frontal zone are proposed as a mechanism for the generation of mesoscale variability at middepth (1000 m) in the southeastern North Atlantic ...
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    Effect of Sea Surface Temperature–Wind Stress Coupling on Baroclinic Instability in the Ocean 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 004:;page 1092
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: The impact of the observed relationship between sea surface temperature and surface wind stress on baroclinic instability in the ocean is explored using linear theory and a nonlinear model. A simple parameterization of the ...
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    Buoyancy-Forced Downwelling in Boundary Currents 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 012:;page 2704
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: The issue of downwelling resulting from surface buoyancy loss in boundary currents is addressed using a high-resolution, nonhydrostatic numerical model. It is shown that the net downwelling is determined by the change in ...
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    Influences of Precipitation on Water Mass Transformation and Deep Convection 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 010:;page 1684
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: he influences of precipitation on water mass transformation and the strength of the meridional overturning circulation in marginal seas are studied using theoretical and idealized numerical models. Nondimensional equations ...
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    On the Circulation of Atlantic Water in the Arctic Ocean 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 011:;page 2352
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: n idealized eddy-resolving numerical model and an analytic three-layer model are used to develop ideas about what controls the circulation of Atlantic Water in the Arctic Ocean. The numerical model is forced with a surface ...
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    Baroclinic Jets in Confluent Flow 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 006:;page 1054
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: The nonlinear, three-dimensional behavior of baroclinic fronts in a barotropic deformation field is investigated. A major finding is that baroclinic instability of the frontal zone can play an important role in limiting ...
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    Dynamics of the Gulf Stream/Deep Western Boundary Current Crossover. Part II: Low-Frequency Internal Oscillations 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 010:;page 2169
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: A low-frequency oscillation in the Gulf Stream/deep western boundary current (DWBC) system is identified and its influences on several important aspects of the basin-scale circulation are investigated. An eddy-resolving ...
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    Dynamics of the Gulf Stream/Deep Western Boundary Current Crossover. Part I: Entrainment and Recirculation 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 010:;page 2152
    Author(s): Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: A regional primitive equation model is applied to the study of the interaction between the Gulf Stream and the deep western boundary current (DWBC) where they cross at Cape Hatteras. It is found that for a wide range of ...
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