Finite-Difference Approximation of the Potential Vorticity Equation for a Stratified Incompressible Fluid and an Example of its Application for Modeling the Black Sea Circulation. Part I. Finite-Difference Equation of Potential Vorticity of Ideal Fluid
S. G. Demyshev
Marine Hydrophysical Institute of RAS, Sevastopol, Russian Federation
e-mail: demyshev@gmail.com
Abstract
Purpose. The study is purposed at deriving the discrete equations of absolute and potential vorticity for a three-dimensional stratified incompressible fluid as an exact consequence of the finite-difference equations of sea dynamics in the field of a potential mass force in the adiabatic approximation provided that viscosity and diffusion are absent. The properties of two-dimensional projections of the absolute vorticity equation onto coordinate planes and the three-dimensional potential vorticity equation are analyzed.
Methods and Results. In order to determine the discrete analogues of absolute and potential vorticity, an additional grid is introduced, where the finite-difference equations for the components both of absolute and potential vorticity are written down. Two-dimensional analogues of the three-dimensional equation of absolute vorticity on the planes (x, y), (y, z) and (x, z) are obtained; they possess the feature of preserving vorticity, energy and enstrophy (square of vorticity). A discrete equation for potential vorticity of a stratified incompressible fluid is derived from the finite-difference system of three-dimensional equations of sea dynamics in the adiabatic approximation at the absence of viscosity and diffusion.
Conclusions. In the case of a linear equation of state, the discrete equations of absolute vorticity and potential vorticity which are the exact consequence of finite-difference formulation are obtained. The equation of potential vorticity is of a divergent form, and two-dimensional analogues of the absolute vorticity equation on the planes (x, y), (y, z) and (x, z) have two quadratic invariants that provide preservation of the average wave number.
Keywords
discrete equation, dynamics of sea, kinetic energy, vortex, potential vorticity, Ertel invariant
Acknowledgements
The study was carried out with financial support of the Russian Science Foundation grant 23-27-00141.
Original russian text
Original Russian Text © S. G. Demyshev, 2024, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 40, Iss. 2, pp. 165–179 (2024)
For citation
Demyshev, S.G., 2024. Finite-Difference Approximation of the Potential Vorticity Equation for a Stratified Incompressible Fluid and an Example of its Application for Modeling the Black Sea Circulation. Part I. Finite-Difference Equation of Potential Vorticity of Ideal Fluid. Physical Oceanography, 31(2), pp. 149-160.
References
- Rossby, C.-G., 1940. Planetary Flow Patterns in the Atmosphere. Quarterly Journal of the Royal Meteorological Society, 66(S1), pp. 68-87. https://doi.org/10.1002/j.1477-870X.1940.tb00130.x
- Ertel, H., 1942. Ein Neuer Hydrodynamischer Wirbelsatz. Meteorologische Zeitschrift, 59(9), pp. 277-281. https://doi.org/10.1127/0941-2948/2004/0013-0451 (in German).
- Hoskins, B.J., McIntyre, M.E. and Robertson, A.W., 1985. On the Use and Significance of Isentropic Potential Vorticity Maps. Quarterly Journal of the Royal Meteorological Society, 111(470), pp. 877-946. https://doi.org/10.1002/qj.49711147002
- Zhmur, V.V., Novoselova, E.V. and Belonenko, T.V., 2021. Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex. Izvestiya, Atmospheric and Oceanic Physics, 57(6), pp. 632-641. https://doi.org/10.1134/S0001433821050157
- Kapsov, E.I., 2019. Numerical Implementation of an Invariant Scheme for One-Dimensional Shallow Water Equations in Lagrangian Coordinates. Keldysh Institute Preprints, (108), pp. 1-28. https://doi.org/10.20948/prepr-2019-108 (in Russian).
- Bihlo, A. and Popovych, R.O., 2012. Invariant Discretization Schemes for the Shallow-Water Equations. SIAM Journal on Scientific Computing, 34(6), pp. B810-B839. https://doi.org/10.1137/120861187
- Charnyi, S., Heister, T., Olshanskii, M.A. and Rebholz, L.G., 2019. Efficient Discretizations for the EMAC Formulation of the Incompressible Navier–Stokes Equations. Applied Numerical Mathematics, 141, pp. 220-233. https://doi.org/10.1016/j.apnum.2018.11.013
- Sorgentone, C., La Cognata, C. and Nordström, J., 2015. A New High Order Energy and Enstrophy Conserving Arakawa-Like Jacobian Differential Operator. Journal of Computational Physics, 301, pp. 167-177. https://doi.org/10.1016/j.jcp.2015.08.028
- Arakawa, A. and Lamb, V.R., 1981. A Potential Enstrophy and Energy Conserving Scheme for the Shallow Water Equations. Monthly Weather Review, 109(1), pp. 18-36. https://doi.org/10.1175/1520-0493(1981)109%3C0018:APEAEC%3E2.0.CO;2
- Salmon, R., 2005. A General Method for Conserving Quantities Related to Potential Vorticity in Numerical Models. Nonlinearity, 18(5), pp. R1-R16. https://doi.org/10.1088/0951-7715/18/5/R01
- Sugibuchi, Y., Matsuo, T. and Sato, S., 2018. Constructing Invariant-Preserving Numerical Schemes Based on Poisson and Nambu Brackets. JSIAM Letters, 10, pp. 53-56. https://doi.org/10.14495/jsiaml.10.53
- Arakawa, A., 1966. Computational Design for Long-Term Numerical Integration of the Equations of Fluid Motion: Two-Dimensional Incompressible Flow. Part I. Journal of Computational Physics, 1(1), pp. 119-143. https://doi.org/10.1016/0021-9991(66)90015-5
- Demyshev, S.G., 2004. Energy of the Black Sea Climatic Circulation. Part I: Discrete Equations of the Rate of Change of Kinetic and Potential Energy. Meteorologiya i Gidrologiya, (9), pp. 65-80 (in Russian).
- Demyshev, S.G., 2005. Numerical Experiments Aimed at the Comparison of Two Finite-Difference Schemes for the Equations of Motion in a Discrete Model of Hydrodynamics of the Black Sea. Physical Oceanography, 15(5), pp. 299-310. https://doi.org/10.1007/s11110-006-0004-2
- Demyshev, S.G., 2023. Nonlinear Invariants of a Discrete System of the Sea Dynamics Equations in a Quasi-Static Approximation. Physical Oceanography, 30(5), pp. 523-548.