Non-stationary polar wind in presence of magnetosphere convection
Time-depended hydrodynamic model TUBE 7 is used for modeling of field-aligned motions and temperature of polar ionosphere ions taking into account magnetosphere convection. It was shown tube geometry changing have a great influence on basic parameters of polar magnetosphere thermal plasma.
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Banks P. M., Holzer
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The polar wind // J. Geophys. Res. 1968. Vol. 73, №
21. P. 6846—6854....
Shifts of adulterations as the result of seasonal horizontal convection under the shelf plate (numerical modeling)
The article shows that the water dynamics induced by differential cooling in upper shelf area (down to 60 m depth) is significantly influenced by day/night variations which delays an establishing of a seasonal water-exchange in shallows. Convective exchange flows within the entire shelf region in seasonal circle requires 4—7 weeks to reach a quasisteady state. Formation of a linear portion on the horizontal temperature profile can be used as an indicator of the approaching of the flow ...
A model of mid-scale irregularities of the low-latitude Earth ionosphere : evaluations of a non-linear correction method for the Z-scheme
A nonlinear correction of the finite-differential scheme for solution of the cross convection-diffusion equations within models of the Rayleigh — Taylor instability in the equatorial region of the Earth ionosphere is considered. For test problems the experimental value of the approximation order of the offered method of non-linear correction of the finite-differential scheme for different types of limiters is received numerically.
1. Гайдуков В. Ю., Кащенко Н. М., Мациевский...
Use of the Z-scheme in an Rayleigh-Taylor instability model
A nonlinear finite-differential scheme for solution of convection-diffusion equation in the field of models of Rayleigh-Taylor instability in the equatorial region of Earth ionosphere is considered. For test tasks monotony of the constructed scheme is in number confirmed. Experimental value of an order of approximation of the offered method of nonlinear correction of the finitedifferential scheme is received.
1. Гайдуков В. Ю., Кащенко Н. М., Мациевский С. В. и...
Three-dimensional computational modelling of water cooling over the coastal slope: a comparison of hydrostatic and non-hydrostatic solutions
... gradients.
1. MIKE3 — User Guide. DHI Water & Environment. DHI Software 2005.
2. Holton J. R. An introduction to dynamic meteorology. 3rd ed. Academic Press,1992.
Chubarenko I. P., Paliy A. A.
hydrodynamics, modelling, hydrostatics, non-hydrostatics, convection,
submarine slope.
65-68
Dependence of the equilibrium state from initial data in numerical global ocean climate model
... вод с временным масштабом ледникового периода // Оптика атмосферы и океана. 2011. Т. 24, № 8.С. 722—725.
Scherbakov A.
numerical model, climate of the ocean, the established state, convection parameterization.
61-67