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    Inertial Oscillations in Geostrophic Flow: Is the Inertial Frequency Shifted by ζ/2 or by ζ? 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 005:;page 884
    Author(s): Chavanne, Cédric P.; Firing, Eric; Ascani, François
    Publisher: American Meteorological Society
    Abstract: he short answer to the question posed in the title is that it depends on the frame of reference chosen to describe the motions. In the inertial limit, the frequency in a rotating frame of reference corresponds to the ...
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    The Deep Equatorial Ocean Circulation in Wind-Forced Numerical Solutions 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 006:;page 1709
    Author(s): Ascani, François; Firing, Eric; McCreary, Julian P.; Brandt, Peter; Greatbatch, Richard J.
    Publisher: American Meteorological Society
    Abstract: e perform eddy-resolving and high vertical resolution numerical simulations of the circulation in an idealized equatorial Atlantic Ocean in order to explore the formation of the deep equatorial circulation (DEC) in this ...
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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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    Deep Equatorial Ocean Circulation Induced by a Forced–Dissipated Yanai Beam 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 005:;page 1118
    Author(s): Ascani, François; Firing, Eric; Dutrieux, Pierre; McCreary, Julian P.; Ishida, Akio
    Publisher: American Meteorological Society
    Abstract: A complex pattern of zonal currents below the thermocline has been observed in the equatorial Pacific and Atlantic Oceans. The currents have typical speeds from 10 to 15 cm s?1 and extend as deep as 2500 m. Their structure ...
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