Zobrazeno 1 - 5
of 5
pro vyhledávání: '"D. N. Elkin"'
Publikováno v:
Journal of Oceanological Research. :5-35
In this work, by means of laboratory modeling, the patterns of evolution (baroclinic instability and/or viscous degeneration) of mesoscale non-frontal baroclinic eddies, or open ocean eddies (without a core with the water of different density) were r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c34469bbb2eb198dcf736c2d0d0b2b6
https://doi.org/10.29006/1564-2291.jor-2023.51(1).1
https://doi.org/10.29006/1564-2291.jor-2023.51(1).1
Autor:
A. G. Zatsepin, D. N. Elkin
Publikováno v:
Physical Oceanography, Vol 25, Iss 3, Pp 165-176 (2018)
Laboratory experiments on studying the downwelling coastal current above the inclined bottom are conducted in the tank placed at a rotating platform. The current is formed by a source of constant flow of water with the same density (barotropic case)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9170c126569c2c2989a164b072ac02ec
http://physical-oceanography.ru/repository/2018/3/en_201803_01.pdf
http://physical-oceanography.ru/repository/2018/3/en_201803_01.pdf
Publikováno v:
Oceanology. 57:478-484
Laboratory experiments on the dynamics of a downwelling coastal current over a sloping bottom were conducted in a tank on a rotating platform. The current was generated by a source of stable water flow of the same density (barotropic case) or of less
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4394432a92c68feb68ee13f05f82d614
https://doi.org/10.1134/s0001437017040051
https://doi.org/10.1134/s0001437017040051
Autor:
A. G. Zatsepin, D. N. Elkin
Publikováno v:
Океанология. 54:614-621
A laboratory study of the alongshore current shear instability in a rotating and nonrotating homogeneous fluid was carried out with special attention paid to the conditions of the coherent eddy structure formation in a shear flow. The cases with both
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eb2a8b2257e916c9a42841ed7aeaabe6
https://doi.org/10.7868/s0030157414050049
https://doi.org/10.7868/s0030157414050049
Autor:
A. G. Zatsepin, D. N. Elkin
Publikováno v:
Oceanology. 53:24-35
The observations carried out in the Caucasian sector of the Black Sea have shown that, under certain conditions, the Rim Current detaches from the coast behind Cape Idocopas. In these cases, an anticyclonic eddy is formed between the detached Rim Cur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11ae70cff5a4e6a3af747a80bc4fd0a0
https://doi.org/10.1134/s0001437012050062
https://doi.org/10.1134/s0001437012050062