The Impact of Abyssal Hill Roughness on the Benthic Tide

Abstract The flow of tides over rough bathymetry in the deep ocean generates baroclinic motion including internal waves and bottom‐trapped tides. The stresses generated by this motion feedback on the amplitude and phase of the large‐scale tide. Quantifying the stresses associated with tidal flow ove...

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Autores principales: Callum J. Shakespeare, Brian K. Arbic, Andrew McC. Hogg
Formato: article
Lenguaje:EN
Publicado: American Geophysical Union (AGU) 2021
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Acceso en línea:https://doaj.org/article/7b985f9d68e3442dbf7788561dc7749d
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