Open AccessParameterization of Mixed Layer and Deep-Ocean Mesoscales including Nonlinearity
Author(s) -
V. M. Canuto,
Yafang Cheng,
M. S. Dubovikov,
A. M. Howard,
Anthony Leboissetier
Publication year - 2018
Publication title -
journal of physical oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.706
H-Index - 143
eISSN - 1520-0485
pISSN - 0022-3670
DOI - 10.1175/jpo-d-16-0255.1
Subject(s) - mesoscale meteorology , isopycnal , forcing (mathematics) , nonlinear system , baroclinity , mixed layer , adiabatic process , geology , ocean dynamics , mean flow , diabatic , stratification (seeds) , altimeter , meteorology , frontogenesis , pycnocline , physics , climatology , ocean current , turbulence , oceanography , thermodynamics , seed dormancy , germination , botany , dormancy , biology , quantum mechanics
In 2011, Chelton et al. carried out a comprehensive census of mesoscales using altimetry data and reached the following conclusions: “essentially all of the observed mesoscale features are nonlinear” and “mesoscales do not move with the mean velocity but with their own drift velocity,” which is “the most germane of all the nonlinear metrics.” Accounting for these results in a mesoscale parameterization presents conceptual and practical challenges since linear analysis is no longer usable and one needs a model of nonlinearity. A mesoscale parameterization is presented that has the following features: 1) it is based on the solutions of the nonlinear mesoscale dynamical equations, 2) it describes arbitrary tracers, 3) it includes adiabatic ( A ) and diabatic ( D ) regimes, 4) the eddy-induced velocity is the sum of a Gent and McWilliams (GM) term plus a new term representing the difference between drift and mean velocities, 5) the new term lowers the transfer of mean potential energy to mesoscales, 6) the isopycnal slopes are not as flat as in the GM case, 7) deep-ocean stratification is enhanced compared to previous parameterizations where being more weakly stratified allowed a large heat uptake that is not observed, 8) the strength of the Deacon cell is reduced. The numerical results are from a stand-alone ocean code with Coordinated Ocean-Ice Reference Experiment I (CORE-I) normal-year forcing.