Conditions for Transformation of a Mesoscale Vortex into a Submesoscale Vortex Filament When the Vortex Is Stretched by an Inhomogeneous Barotropic Flow

Author:

Zhmur V. V.,Belonenko T. V.,Novoselova E. V.,Suetin B. P.

Publisher

Pleiades Publishing Ltd

Subject

Oceanography

Reference21 articles.

1. G. I. Barenblatt, Similarity, Self-Similarity, and Intermediate Asymptotics (Gidrometeoizdat, Leningrad, 1978) [in Russian].

2. V. V. Zhmur, Mesoscale Ocean Eddies (GEOS, Moscow, 2011) [in Russian].

3. V. V. Zhmur, E. V. Novoselova, and T. V. Belonenko, “Potential vorticity in the ocean: Ertel and Rossby approaches with estimates for the Lofoten vortex,” Izv., Atmos. Ocean. Phys. 57 (6), 632–641 (2021). https://doi.org/10.1134/S0001433821050157

4. V. V. Zhmur, E. V. Novoselova, and T. V. Belonenko, “Peculiarities of formation of the density field in mesoscale eddies of the Lofoten Basin: Part 2,” Oceanology 62 (3), 289–302 (2022). https://doi.org/10.1134/S0001437022030171

5. V. V. Zhmur and K. K. Pankratov, “Dynamics of an ellipsoidal near-surface vortex in an inhomogeneous flow,” Okeanologiya 29 (2), 205–211 (1989).

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