Standard

Волны или вихри? / Belonenko, T. V.; Zakharchuk, E. A.; Fux, V. R.

в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, № 3, 1998, стр. 37-44.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Belonenko, TV, Zakharchuk, EA & Fux, VR 1998, 'Волны или вихри?', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, № 3, стр. 37-44.

APA

Belonenko, T. V., Zakharchuk, E. A., & Fux, V. R. (1998). Волны или вихри? ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, (3), 37-44.

Vancouver

Belonenko TV, Zakharchuk EA, Fux VR. Волны или вихри? ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 1998;(3):37-44.

Author

Belonenko, T. V. ; Zakharchuk, E. A. ; Fux, V. R. / Волны или вихри?. в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 1998 ; № 3. стр. 37-44.

BibTeX

@article{ce025789951b4e7e916e86fdf27747eb,
title = "Волны или вихри?",
abstract = "The paper discusses an issue of difference between relative energy inputs from vortexes and low-frequency waves in the sea. Two phenomenological models are considered: a synoptical vortex and a low-frequency wave, where the level rise is analytically prescribed and the flow speed is calculated by hydro-dynamical equation taken in the linear quasi-geostrophical approximation. It is shown that under the pattern of spatial/temporal variation of the observed currents.",
author = "Belonenko, {T. V.} and Zakharchuk, {E. A.} and Fux, {V. R.}",
year = "1998",
language = "русский",
pages = "37--44",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "3",

}

RIS

TY - JOUR

T1 - Волны или вихри?

AU - Belonenko, T. V.

AU - Zakharchuk, E. A.

AU - Fux, V. R.

PY - 1998

Y1 - 1998

N2 - The paper discusses an issue of difference between relative energy inputs from vortexes and low-frequency waves in the sea. Two phenomenological models are considered: a synoptical vortex and a low-frequency wave, where the level rise is analytically prescribed and the flow speed is calculated by hydro-dynamical equation taken in the linear quasi-geostrophical approximation. It is shown that under the pattern of spatial/temporal variation of the observed currents.

AB - The paper discusses an issue of difference between relative energy inputs from vortexes and low-frequency waves in the sea. Two phenomenological models are considered: a synoptical vortex and a low-frequency wave, where the level rise is analytically prescribed and the flow speed is calculated by hydro-dynamical equation taken in the linear quasi-geostrophical approximation. It is shown that under the pattern of spatial/temporal variation of the observed currents.

UR - http://www.scopus.com/inward/record.url?scp=0032451234&partnerID=8YFLogxK

M3 - статья

SP - 37

EP - 44

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 3

ER -

ID: 5016772