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    The Effects of Friction and β on Finite-Amplitude Baroclinic Waves 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 011:;page 1689
    Author(s): Romea, Richard D.
    Publisher: American Meteorological Society
    Abstract: A linear and finite-amplitude analysis of the baroclinic instability of a zonal current is presented. Both the ? effect and viscosity are included. A small but finite amount of dissipation destabilizes the system, lowering ...
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    Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part I: Observations 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 011:;page 2091
    Author(s): Hsueh, Y.; Romea, Richard D.
    Publisher: American Meteorological Society
    Abstract: Analyses of low-pass filtered coastal sea-level data and geostrophic winds derived from surface pressure charts for the period of 1 December 1980 through 31 March 1981 indicate that the wintertime dynamics in the Northeast ...
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    Further Evidence for Coastal Trapped Waves along the Peru Coast 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 008:;page 1341
    Author(s): Romea, Richard D.; Smith, Robert L.
    Publisher: American Meteorological Society
    Abstract: Time series of coastal sea level during 1976?77, from 2°12?S to 17°S along the west coast of South America, show that low-frequency, ? < 0.25 cycles per day (cpd), fluctuations propagate poleward with the phase speed of ...
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    Wintertime Winds and Coastal Sea-Level Fluctuations in the Northeast China Sea. Part II: Numerical Model 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 002:;page 241
    Author(s): Hsueh, Y.; Romea, Richard D.; DeWitt, P. W.
    Publisher: American Meteorological Society
    Abstract: As a sequel to data analysis reported in Part I, a numerical model of the wintertime wind-driven circulation of the northeast Chine Sea is developed with the primary purpose of achieving an understanding of the underlying ...
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