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    The Sea Level Response of a Stratified Ocean to Barometric Pressure Forcing 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 001:;page 109
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: The nature of the sea surface adjustment to atmospheric loading in a stratified ocean is examined for both midlatitude and equatorial regions, using simple analytical solutions to the quasigeostrophic and equatorial ?-plane ...
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    Rate of Work Done by Atmospheric Pressure on the Ocean General Circulation and Tides 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 002:;page 458
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: Quantitative analysis of the energetics of the ocean is crucial for understanding its circulation and mixing. The power input by fluctuations in atmospheric pressure pa resulting from the S1 and S2 air tides and the ...
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    Nonequilibrium Response of the Global Ocean to the 5-Day Rossby–Haurwitz Wave in Atmospheric Surface Pressure 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010:;page 2158
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: The response of the global ocean to the surface pressure signal associated with the well-known 5-day Rossby?Haurwitz atmospheric mode is explored using analytical and numerical tools. Solutions of the Laplace tidal equations ...
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    Viscid Eastern Boundary Dynamics and the Spreading of Mediterranean Water along the Portuguese Continental Slope 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 010:;page 2437
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: A linear, continuously stratified model is used to investigate the flows generated by a midlatitude, eastern boundary zonal inflow representing the flux of Mediterranean Water into the North Atlantic. The model allows for ...
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    A Simple Model for Deep Equatorial Zonal Currents Forced at Lateral Boundaries 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 012:;page 1881
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: Deep lateral boundary processes (e.g., western boundary currents) are hypothesized as an alternative energy source exciting the equatorial wave guide at long time scales. A linear, continuously stratified model is used to ...
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    Oceanic Response to Surface Loading Effects Neglected in Volume-Conserving Models 

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 003:;page 426
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: Forcing by freshwater fluxes implies variable surface loads that are not treated in volume-conserving ocean models. A similar problem exists with the representation of volume changes implied by surface heat fluxes. Under ...
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    Low-Frequency Sea Level Variability and the Inverted Barometer Effect 

    Source: Journal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 004:;page 619
    Author(s): Ponte, Rui M.
    Publisher: American Meteorological Society
    Abstract: For a dynamical interpretation of sea level records, estimates are needed of the isostatic, or so-called inverted barometer, signals (?ib) associated with the ocean response to atmospheric loading. Seasonal and longer-period ...
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    Effects of Unresolved High-Frequency Signals in Altimeter Records Inferred from Tide Gauge Data 

    Source: Journal of Atmospheric and Oceanic Technology:;2002:;volume( 019 ):;issue: 004:;page 534
    Author(s): Ponte, Rui M.; Lyard, Florent
    Publisher: American Meteorological Society
    Abstract: Rapid sea level signals are poorly resolved, or ?aliased,? by the TOPEX/Poseidon altimeter, due to its ?10-day repeat cycle (Nyquist period TN ? 20 days). To assess the potential for temporal aliasing in the altimeter data, ...
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    Propagating Bottom Pressure Signals around Antarctica at 1–2-Day Periods and Implications for Ocean Modes 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 001:;page 284
    Author(s): Ponte, Rui M.; Hirose, Naoki
    Publisher: American Meteorological Society
    Abstract: Previous studies of barotropic ocean dynamics have shown that several global normal modes are possible at periods between 1 and 2 days. The role of these modes in diurnal tidal dynamics is well documented, but finding ...
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    Analysis and Interpretation of Deep Equatorial Currents in the Central Pacific 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 008:;page 1025
    Author(s): Ponte, Rui M.; Luyten, James
    Publisher: American Meteorological Society
    Abstract: Analysis of vertical profiles of absolute horizontal velocity collected in January 1981, February and April 1982 in the equatorial central Pacific revealed two significant narrowband spectral peaks in zonal velocity, ...
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