A parameterization of local and remote tidal mixing
- Casimir de Lavergne,
- Clément Vic,
- Gurvan Madec,
- Fabien Roquet,
- Amy Waterhouse,
- Caitlin Whalen,
- Yannis Cuypers,
- Pascale Bouruet-Aubertot,
- Bruno Ferron,
- Toshiyuki Hibiya
Clément Vic
LOPS Laboratory, UBO-IFREMER-CNRS-IRD, Plouzané, France
Author ProfileGurvan Madec
LOCEAN Laboratory, Sorbonne Université-CNRS-IRD-MNHN, Paris, France
Author ProfileFabien Roquet
Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden
Author ProfileAmy Waterhouse
Scripps Institution of Oceanography, University of California, La Jolla, California
Author ProfileCaitlin Whalen
Applied Physics Laboratory, University of Washington, Seattle, Washington
Author ProfileYannis Cuypers
LOCEAN Laboratory, Sorbonne Université-CNRS-IRD-MNHN, Paris, France
Author ProfilePascale Bouruet-Aubertot
LOCEAN Laboratory, Sorbonne Université-CNRS-IRD-MNHN, Paris, France
Author ProfileBruno Ferron
LOPS Laboratory, UBO-IFREMER-CNRS-IRD, Plouzané, France
Author ProfileToshiyuki Hibiya
Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, Tokyo, Japan
Author ProfileAbstract
Vertical mixing is often regarded as the Achilles' heel of ocean models.
In particular, few models include a comprehensive and energy-constrained
parameterization of mixing by internal ocean tides. Here, we present an
energy-conserving mixing scheme which accounts for the local breaking of
high-mode internal tides and the distant dissipation of low-mode
internal tides. The scheme relies on four static two-dimensional maps of
internal tide dissipation, constructed using mode-by-mode Lagrangian
tracking of energy beams from sources to sinks. Each map is associated
with a distinct dissipative process and a corresponding vertical
structure. Applied to an observational climatology of stratification,
the scheme produces a global three-dimensional map of dissipation which
compares well with available microstructure observations and with
upper-ocean finestructure mixing estimates. This relative agreement,
both in magnitude and spatial structure across ocean basins, suggests
that internal tides underpin most of observed dissipation in the ocean
interior at the global scale. The proposed parameterization is therefore
expected to improve understanding, mapping and modelling of ocean
mixing.May 2020Published in Journal of Advances in Modeling Earth Systems volume 12 issue 5. 10.1029/2020MS002065