Two-Layer Ocean Circulation Model with Variational Control of Turbulent Viscosity Coefficient

[1] Volkov E. A.(1997)“On the solution of a modified Dirichlet problem on a multiconnected polygon by the rapid block method,” Tr. Mat. Inst Steklova 214 135-144

[2] Zalesny V. B.(2022)“Variation method for solving the quasi-geostrophic circulation problem in a two-layer ocean,” Izv Fiz. Atmos. Ocean. Phys. 58 423-432

[3] Ivchenko V. O.(2019)“Diffusion–rotational parameterization of eddy fluxes of potential vorticity: Barotropic flow in the zonal channel,” Izv Fiz. Atmos. Ocean. Phys. 55 1-16

[4] Zalesny V. B.(1961)On the integration of equations of the theory of sea currents in nonsimply connected domains Dokl. Akad. Nauk SSSR 138 1076-1079

[5] Kamenkovich V. M.(2019)“Methods for observation data assimilation in problems of physics of atmosphere and ocean,” Izv Fiz. Atmos. Ocean. Phys. 55 17-31

[6] Shutyaev V. P.(2010)Convergence of solutions to the problem of data assimilation for a multilayer quasigeostrophic model of ocean dynamics Russ. J. Numer. Anal. Math. Modell. 25 105-115

[7] Agoshkov V. I.(1994)Existence of attractor for the quasi-geostrophic approximation of the Navier–Stokes equations and estimate of its dimension Adv. Math. Sci. Appl. 4 465-489

[8] Ipatova V. M.(2000)“The finiteness of determining degrees of freedom for the quasi-geostrophic multi-layer ocean model,” Nonlinear Anal. Theory Methods Appl. 42 1499-1512

[9] Bernier C.(1981)Comparison of a barotropic blocking theory with observation J. Atmos. Sci. 38 762-779

[10] Bernier C.(2022)Transitions of zonal flows in a two-layer quasi-geostrophic ocean model Nonlinear Dyn. 109 1887-1904

[1] Volkov E. A.(1997)“On the solution of a modified Dirichlet problem on a multiconnected polygon by the rapid block method,” Tr. Mat. Inst Steklova 214 135-144

[2] Zalesny V. B.(2022)“Variation method for solving the quasi-geostrophic circulation problem in a two-layer ocean,” Izv Fiz. Atmos. Ocean. Phys. 58 423-432

[3] Ivchenko V. O.(2019)“Diffusion–rotational parameterization of eddy fluxes of potential vorticity: Barotropic flow in the zonal channel,” Izv Fiz. Atmos. Ocean. Phys. 55 1-16

[4] Zalesny V. B.(1961)On the integration of equations of the theory of sea currents in nonsimply connected domains Dokl. Akad. Nauk SSSR 138 1076-1079

[5] Kamenkovich V. M.(2019)“Methods for observation data assimilation in problems of physics of atmosphere and ocean,” Izv Fiz. Atmos. Ocean. Phys. 55 17-31

[6] Shutyaev V. P.(2010)Convergence of solutions to the problem of data assimilation for a multilayer quasigeostrophic model of ocean dynamics Russ. J. Numer. Anal. Math. Modell. 25 105-115

[7] Agoshkov V. I.(1994)Existence of attractor for the quasi-geostrophic approximation of the Navier–Stokes equations and estimate of its dimension Adv. Math. Sci. Appl. 4 465-489

[8] Ipatova V. M.(2000)“The finiteness of determining degrees of freedom for the quasi-geostrophic multi-layer ocean model,” Nonlinear Anal. Theory Methods Appl. 42 1499-1512

[9] Bernier C.(1981)Comparison of a barotropic blocking theory with observation J. Atmos. Sci. 38 762-779

[10] Bernier C.(2022)Transitions of zonal flows in a two-layer quasi-geostrophic ocean model Nonlinear Dyn. 109 1887-1904