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Observations of the Low‐Mode Internal Tide and Its Interaction With Mesoscale Flow South of the Azores
Author(s) -
Löb Jonas,
Köhler Janna,
Mertens Christian,
Walter Maren,
Li Zhuhua,
Storch JinSong,
Zhao Zhongxiang,
Rhein Monika
Publication year - 2020
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2019jc015879
Subject(s) - energy flux , eddy , mesoscale meteorology , dissipation , internal tide , energy flow , flux (metallurgy) , internal wave , climatology , energy budget , atmospheric sciences , mode (computer interface) , coherence (philosophical gambling strategy) , forcing (mathematics) , satellite , geology , geophysics , physics , mechanics , energy (signal processing) , turbulence , materials science , astronomy , quantum mechanics , computer science , metallurgy , thermodynamics , operating system
Understanding the temporal variability of internal tides plays a crucial role in identifying sources and sinks of energy in the ocean. Using a 10‐month‐long time series from moored instruments inside a tidal beam south of the Azores, the magnitude and the underlying causes of temporal variability in the first two modes of the internal tide energy flux was studied. We analyzed changes of the direction and coherence of the energy flux, its modal structure, and the impact of two eddies. Semidiurnal energy fluxes were further compared with estimates from a 1/10° ocean global circulation model, as well as with fluxes derived from satellite altimetry. All energy fluxes correlate reasonably well in direction, deviations from its fixed phase relation to astronomical forcing, and modal composition while model and satellite underestimate the total energy flux. A pronounced damping of the in situ fluxes coincides with the passing of two eddies. In the presence of a surface‐intensified eddy, the coherent part of the energy flux in the first two modes is lowered by more than 40%, a subsurface eddy coincides with a decrease of the energy flux mainly in the second mode. These observations support the hypothesis that eddy interactions increase the incoherent part of the energy flux and transfer energy from low modes into higher modes, which can lead to increased local dissipation. It remains an open question how much of the energy converted from lower to higher modes results in local dissipation, a crucial part in creating energetically consistent ocean‐climate models.