Modeling the origin and evolution of convective vortex structures on a slope. Numerical experiment
https://doi.org/10.59887/2073-6673.2025.18(4)-2
EDN: EISBND
Abstract
A detailed non-hydrostatic model of gravitational flow over an inclined bottom is being developed, which is capable of explicitly reproduce convective cells for future generalization and new parameterizations development. To minimize numerical noise, the method of an inclined computational domain and a regular rectangular grid are used. The properties of high-order accurate advection schemes are investigated. The fundamental possibility of explicitly numerical reproduction of relatively large (on the order of a meter or more) ocean turbulent structures, such as convective cells, is demonstrated. A high-resolution digital array of 3-dimensional velocity and tracer fields (active and passive) created based on a physical experiment for a range of Reynolds numbers of 30–300. This array will be used to develop new parameterizations for a large-scale ocean circulation model.
About the Authors
R. Ye. VankevichRussian Federation
Scopus AuthorID: 25642198100, WoS ResearcherID: M-3215-2013
36 Nakhimovsky Prosp., Moscow 117997
А. А. Rodionov
Russian Federation
Scopus AuthorID: 56223713100, WoS ResearcherID: AAT-6466-2021
36 Nakhimovsky Prosp., Moscow 117997
N. N. Shpilev
Russian Federation
36 Nakhimovsky Prosp., Moscow 117997
V. V. Chebotkova
Russian Federation
36 Nakhimovsky Prosp., Moscow 117997
References
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Review
For citations:
Vankevich R.Ye., Rodionov А.А., Shpilev N.N., Chebotkova V.V. Modeling the origin and evolution of convective vortex structures on a slope. Numerical experiment. Fundamental and Applied Hydrophysics. 2025;18(4):20-27. (In Russ.) https://doi.org/10.59887/2073-6673.2025.18(4)-2. EDN: EISBND























