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    The Completeness of Eigenfunctions of the Tidal Equation on an Equatorial Beta Plane 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 006:;page 769
    Author(s): Wu, Zhaohua; Moore, Dennis W.
    Publisher: American Meteorological Society
    Abstract: The approximate tidal theory on an equatorial beta plane has been widely applied to tropical atmospheric dynamics. There are many successful examples of such applications. However, the mathematical and physical origin of ...
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    The Pacific Subsurface Countercurrents and an Inertial Model 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 011:;page 2448
    Author(s): Johnson, Gregory C.; Moore, Dennis W.
    Publisher: American Meteorological Society
    Abstract: The Tsuchiya jets, or subsurface countercurrents, extend across the Pacific Ocean carrying 7 (±2) ? 106 m3 s?1 eastward on each side of the equator. Mean meridional sections of potential temperature, salinity, neutral ...
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    A Note on Low-Frequency Equatorial Basin Modes 

    Source: Journal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 011:;page 1578
    Author(s): Cane, Mark A.; Moore, Dennis W.
    Publisher: American Meteorological Society
    Abstract: A new low-frequency standing equatorial wave mode is described. It is composed solely of long Kelvin and Rossby waves, whereas previously described low-frequency modes involved short, eastward propagating Rossby waves. It ...
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    Exact Solutions to Kawase's Linear Model of Deep Ocean Circulation 

    Source: Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 010:;page 2188
    Author(s): Wang, Dailin; Moore, Dennis W.; Rothstein, Lewis M.
    Publisher: American Meteorological Society
    Abstract: Exact solutions are found for Kawase's linear, two-layer model of mass-driven deep-ocean circulation. It is demonstrated that for strong damping, even though the deep western boundary current (DWBC) bifurcates at the equator ...
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    Sverdrup and Nonlinear Dynamics of the Pacific Equatorial Currents 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 005:;page 994
    Author(s): Kessler, William S.; Johnson, Gregory C.; Moore, Dennis W.
    Publisher: American Meteorological Society
    Abstract: The Sverdrup circulation in the tropical Pacific is constructed from satellite scatterometer winds, compared with measured ocean currents, and diagnosed in an ocean GCM. Previous depictions of the Sverdrup circulation near ...
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    Interior Reflections of a Periodically Forced Equatorial Kelvin Wave 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 007:;page 985
    Author(s): Rothstein, Lewis M.; Moore, Dennis W.; McCreary, Julian P.
    Publisher: American Meteorological Society
    Abstract: A fully three-dimensional, wind-forced equatorial model is used to study the effects of the strong near- surface equatorial pycnocline on energy transmission into the deep ocean. The equatorial Kelvin waves forced by a ...
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    Temporal and Spatial Structure of the Equatorial Deep Jets in the Pacific Ocean 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 012:;page 3396
    Author(s): Johnson, Gregory C.; Kunze, Eric; McTaggart, Kristene E.; Moore, Dennis W.
    Publisher: American Meteorological Society
    Abstract: The spatial and temporal structure of the equatorial deep jets (EDJs) in the Pacific Ocean is investigated using CTD station data taken on the equator from 1979 through 2001. The EDJs are revealed in profiles of vertical ...
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    Comments on “A Theory of Equatorial Deep Jets” 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007:;page 1781
    Author(s): Ascani, François; Wang, Dailin; Moore, Dennis W.; Firing, Eric; McCreary, Julian P.
    Publisher: American Meteorological Society
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