Zobrazeno 1 - 10
of 28
pro vyhledávání: '"V. B. Zalesny"'
Autor:
R. Marsh, V. O. Ivchenko, N. Skliris, S. Alderson, G. R. Bigg, G. Madec, A. T. Blaker, Y. Aksenov, B. Sinha, A. C. Coward, J. Le Sommer, N. Merino, V. B. Zalesny
Publikováno v:
Geoscientific Model Development, Vol 8, Iss 5, Pp 1547-1562 (2015)
An established iceberg module, ICB, is used interactively with the Nucleus for European Modelling of the Ocean (NEMO) ocean model in a new implementation, NEMO–ICB (v1.0). A 30-year hindcast (1976–2005) simulation with an eddy-permitting (0.25°)
Externí odkaz:
https://doaj.org/article/6f4b959bdf084e4a8662d3d237cd0117
Autor:
V. B. Zalesny
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 59:189-200
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33155bd8cbd0d42f8cc71bef37f8a06e
https://doi.org/10.1134/s000143382302010x
https://doi.org/10.1134/s000143382302010x
Autor:
V. B. Zalesny
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 58:423-432
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::054b76e2b4ea2b1b21b702a580e685a2
https://doi.org/10.1134/s0001433822050139
https://doi.org/10.1134/s0001433822050139
Autor:
V. B. Zalesny, S. N. Moshonkin
Publikováno v:
Известия Российской академии наук. Физика атмосферы и океана. 55:103-113
Ocean general circulation model (OGCM) of the INM RAS with embedded k turbulent model is developed. The solution of the k model equations depends on the frequencies of buoyancy and velocity shift which are generated by the OGCM. The coefficients of v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ce133e47181ab881f4d3b34d3464fb7
https://doi.org/10.31857/s0002-3515555103-113
https://doi.org/10.31857/s0002-3515555103-113
Autor:
V. O. Ivchenko, V. B. Zalesny
Publikováno v:
Известия Российской академии наук. Физика атмосферы и океана. 55:3-16
The problem of parametrization of the eddy fluxes of a potential vorticity is discussed. Traditional diffusion parameterization is complemented by the inclusion of a rotational component. For the analysis of the new scheme, a quasi-geostrophic model
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23e1bcb874b99192a67d064932f4faf2
https://doi.org/10.31857/s0002-35155513-16
https://doi.org/10.31857/s0002-35155513-16
Publikováno v:
Journal of Physics: Conference Series. 1392:012046
To solve the problems of large-scale dynamics of the atmosphere and the ocean, a system of single-layer two-dimensional shallow water equations on a sphere is often used [1, 2]. Such a system is the basis for solving complete baroclinic systems of pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f18d3ce7f7ae825dfc0e895414634ced
https://doi.org/10.1088/1742-6596/1392/1/012046
https://doi.org/10.1088/1742-6596/1392/1/012046
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 231:012038
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abce532175dcbf55a5be5fcc4e052853
https://doi.org/10.1088/1755-1315/231/1/012038
https://doi.org/10.1088/1755-1315/231/1/012038
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 49:579-591
An analysis is given of the methods of operational oceanography based on measurements derived from satellite data, observations acquired by drifters and passing vessels, and modern simulations of marine and oceanic circulations. In addition, a histor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49c3ecbaf359256a99ad5976db353059
https://doi.org/10.1134/s000143381306011x
https://doi.org/10.1134/s000143381306011x
Publikováno v:
Doklady Earth Sciences. 443:426-430
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1238e0f8e2789a1043fccf9d6e78eeea
https://doi.org/10.1134/s1028334x1203021x
https://doi.org/10.1134/s1028334x1203021x
Autor:
V. I. Agoshkov, V. B. Zalesny
Publikováno v:
Pure and Applied Geophysics. 169:555-578
Problems of the variational data assimilation for the primitive equation ocean model constructed at the Institute of Numerical Mathematics, Russian Academy of Sciences are considered. The model has a flexible computational structure and consists of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91af17cbcfbb0fd1a2bd7506492f4681
https://doi.org/10.1007/s00024-011-0372-5
https://doi.org/10.1007/s00024-011-0372-5