Baroclinic Motions and Energetics as Measured by Altimeters

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Baroclinic Motions and Energetics as Measured by Altimeters

Small surface displacements appearing in tide gauge and altimetric records are used to detect hydrostatic baroclinic modes in the ocean. Those deflections are a small fraction of the interior isopycnal vertical displacements and are dependent directly upon the in situ stratification. Conversion of surface height to interior amplitudes and energies encounters significant spatial and seasonal shi...

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ژورنال

عنوان ژورنال: Journal of Atmospheric and Oceanic Technology

سال: 2013

ISSN: 0739-0572,1520-0426

DOI: 10.1175/jtech-d-12-00035.1