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Semidiurnal Internal Tide Energy Fluxes And Their Variability In A Global Ocean Model And Moored Observations

Title: Semidiurnal Internal Tide Energy Fluxes And Their Variability In A Global Ocean Model And Moored Observations.
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Name(s): Ansong, Joseph K., author
Arbic, Brian K., author
Alford, Matthew H., author
Buijsman, Maarten C., author
Shriver, Jay F., author
Zhao, Zhongxiang, author
Richman, James G., author
Simmons, Harper L., author
Timko, Patrick G., author
Wallcraft, Alan J., author
Zamudio, Luis, author
Type of Resource: text
Genre: Journal Article
Text
Journal Article
Date Issued: 2017-03
Physical Form: computer
online resource
Extent: 1 online resource
Language(s): English
Abstract/Description: We examine the temporal means and variability of the semidiurnal internal tide energy fluxes in 1/25 degrees global simulations of the Hybrid Coordinate Ocean Model (HYCOM) and in a global archive of 79 historical moorings. Low-frequency flows, a major cause of internal tide variability, have comparable kinetic energies at the mooring sites in model and observations. The computed root-mean-square (RMS) variability of the energy flux is large in both model and observations and correlates positively with the time-averaged flux magnitude. Outside of strong generation regions, the normalized RMS variability (the RMS variability divided by the mean) is nearly independent of the flux magnitudes in the model, and of order 23% or more in both the model and observations. The spatially averaged flux magnitudes in observations and the simulation agree to within a factor of about 1.4 and 2.4 for vertical mode-1 and mode-2, respectively. The difference in energy flux computed from the full-depth model output versus model output subsampled at mooring instrument depths is small. The global historical archive is supplemented with six high-vertical resolution moorings from the Internal Waves Across the Pacific (IWAP) experiment. The model fluxes agree more closely with the high-resolution IWAP fluxes than with the historical mooring fluxes. The high variability in internal tide energy fluxes implies that internal tide fluxes computed from short observational records should be regarded as realizations of a highly variable field, not as "means" that are indicative of conditions at the measurement sites over all time.
Identifier: FSU_libsubv1_wos_000400678900015 (IID), 10.1002/2016JC012184 (DOI)
Keywords: accuracy, circulation model, baroclinic tides, deep-ocean, dissipation, general-circulation, hawaiian ridge, philippine sea, surface manifestation, wave drag
Publication Note: The publisher's version of record is available at https://doi.org/10.1002/2016JC012184
Persistent Link to This Record: http://purl.flvc.org/fsu/fd/FSU_libsubv1_wos_000400678900015
Owner Institution: FSU
Is Part Of: Journal of Geophysical Research-Oceans.
2169-9275
Issue: iss. 3, vol. 122

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Ansong, J. K., Arbic, B. K., Alford, M. H., Buijsman, M. C., Shriver, J. F., Zhao, Z., … Zamudio, L. (2017). Semidiurnal Internal Tide Energy Fluxes And Their Variability In A Global Ocean Model And Moored Observations. Journal Of Geophysical Research-Oceans. Retrieved from http://purl.flvc.org/fsu/fd/FSU_libsubv1_wos_000400678900015