We introduce in this paper some elements for the mathematical and numerical analysis of algebraic turbulence models for oceanic surface mixing layers. In these models the turbulent diffusions are parameterized by means of the gradient Richardson number, that measures the balance between stabilizing buoyancy forces and destabilizing shearing forces. We analyze the existence and linear exponential asymptotic stability of continuous and discrete equilibria states. We also analyze the well-posedness of a simplified model, by application of the linearization principle for non-linear parabolic equations. We finally present some numerical tests for realistic flows in tropical seas that reproduce the formation of mixing layers in time scales of the order of days, in agreement with the physics of the problem. We conclude that the typical mixing layers are transient effects due to the variability of equatorial winds. Also, that these states evolve to steady states in time scales of the order of years, under negative surface energy flux conditions.
Mots clés : turbulent mixing layers, Richardson number, first order closure models, conservative numerical solution, stability of steady states, tests for tropical seas
@article{M2AN_2010__44_6_1255_0, author = {Bennis, Anne-Claire and Chac\'on Rebollo, Tomas and G\'omez M\'armol, Macarena and Lewandowski, Roger}, title = {Numerical modelling of algebraic closure models of oceanic turbulent mixing layers}, journal = {ESAIM: Mathematical Modelling and Numerical Analysis }, pages = {1255--1277}, publisher = {EDP-Sciences}, volume = {44}, number = {6}, year = {2010}, doi = {10.1051/m2an/2010025}, mrnumber = {2769057}, language = {en}, url = {http://www.numdam.org/articles/10.1051/m2an/2010025/} }
TY - JOUR AU - Bennis, Anne-Claire AU - Chacón Rebollo, Tomas AU - Gómez Mármol, Macarena AU - Lewandowski, Roger TI - Numerical modelling of algebraic closure models of oceanic turbulent mixing layers JO - ESAIM: Mathematical Modelling and Numerical Analysis PY - 2010 SP - 1255 EP - 1277 VL - 44 IS - 6 PB - EDP-Sciences UR - http://www.numdam.org/articles/10.1051/m2an/2010025/ DO - 10.1051/m2an/2010025 LA - en ID - M2AN_2010__44_6_1255_0 ER -
%0 Journal Article %A Bennis, Anne-Claire %A Chacón Rebollo, Tomas %A Gómez Mármol, Macarena %A Lewandowski, Roger %T Numerical modelling of algebraic closure models of oceanic turbulent mixing layers %J ESAIM: Mathematical Modelling and Numerical Analysis %D 2010 %P 1255-1277 %V 44 %N 6 %I EDP-Sciences %U http://www.numdam.org/articles/10.1051/m2an/2010025/ %R 10.1051/m2an/2010025 %G en %F M2AN_2010__44_6_1255_0
Bennis, Anne-Claire; Chacón Rebollo, Tomas; Gómez Mármol, Macarena; Lewandowski, Roger. Numerical modelling of algebraic closure models of oceanic turbulent mixing layers. ESAIM: Mathematical Modelling and Numerical Analysis , Tome 44 (2010) no. 6, pp. 1255-1277. doi : 10.1051/m2an/2010025. http://www.numdam.org/articles/10.1051/m2an/2010025/
[1] Variability of the tropical atlantic ocean simulated by a general circulation model with two different mixed-layer physics. J. Phys. Oceanogr. 23 (1993) 1363-1388.
and ,[2] On the stability of the l2 projection in h1. Math. Comp. 7 (2001) 147-156. | Zbl
, and ,[3] Applied turbulence modelling in marine water. Ph.D. Thesis, University of Hambourg, Germany (2004). | Zbl
,[4] A simple eddy kinetic energy model for simulations of the oceanic vertical mixing: test at Station Papa and long-term upper ocean study site. J. Geophys. Res. 16 (1990) 179-193.
, and ,[5] The heat budget of the toga-coare domain in an ocean model. J. Geophys. Res. 96 (1991) 3323-3330.
,[6] Sensitivity of a global coupled ocean-sea ice model to the parametrization of vertical mixing. J. Geophys. Res. 104 (1999) 13681-13695.
, , and ,[7] Vertical mixing in the equatorial undercurrent. J. Phys. Oceanogr. 3 (1973) 286-296.
,[8] Numerical modeling of ocean dynamics. World Scientific (1993).
and ,[9] Oceanic vertical mixing: a review and a model with a nonlocal boundary layer parametrization. Rev. Geophys. 32 (1994) 363-403.
, and ,[10] OPA version 8.0, Ocean General Circulation Model Reference Manual. LODYC, Int. Rep. 97/04 (1997).
, , and ,[11] The tropical atmosphere ocean (tao) array is completed. Bull. Am. Meteorol. Soc. 76 (1995) 739-741.
,[12] Development of a turbulence closure model for geophysical fluid problems. Rev. Geophys. Space Phys. 20 (1982) 851-875.
and ,[13] Parametrization of vertical mixing in numericals models of the tropical oceans. J. Phys. Oceanogr. 11 (1981) 1443-1451.
and ,[14] Geophysical fluid dynamics. Springer (1987). | Zbl
,[15] The linearization principle for the stability of solutions of quasilinear parabolic equations. Arch. Ration. Mech. Anal. 77 (1981) 301-320. | Zbl
,[16] An investigation into the wind as the cause of the equatiorial undercurrent. J. Mar. Res. 24 (1966) 179-204.
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