Internal Tide Attenuation in the North Pacific

Abstract Multisatellite altimetry and an eddy‐resolving model with tides are used to quantify the attenuation of the mode‐1 M2 internal tide as it propagates from three major sources in the North Pacific. The model is used to correct the altimetric fluxes for the nonstationary signal that altimeters...

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Bibliographic Details
Main Authors: Matthew H. Alford, Harper L. Simmons, Olavo B. Marques, James B. Girton
Format: Article
Language:English
Published: Wiley 2019-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2019GL082648
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