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Interaction between Rossby Waves and a Jet Flow : Basic Equations and Verification for the Antarctic Circumpolar Current. / Gnevyshev, V. G.; Frolova, A. V.; Kubryakov, A. A.; Sobko, Yu V.; Belonenko, T. V.

в: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Том 55, № 5, 01.09.2019, стр. 412-422.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Gnevyshev, VG, Frolova, AV, Kubryakov, AA, Sobko, YV & Belonenko, TV 2019, 'Interaction between Rossby Waves and a Jet Flow: Basic Equations and Verification for the Antarctic Circumpolar Current', IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Том. 55, № 5, стр. 412-422. https://doi.org/10.1134/S0001433819050074

APA

Gnevyshev, V. G., Frolova, A. V., Kubryakov, A. A., Sobko, Y. V., & Belonenko, T. V. (2019). Interaction between Rossby Waves and a Jet Flow: Basic Equations and Verification for the Antarctic Circumpolar Current. IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, 55(5), 412-422. https://doi.org/10.1134/S0001433819050074

Vancouver

Gnevyshev VG, Frolova AV, Kubryakov AA, Sobko YV, Belonenko TV. Interaction between Rossby Waves and a Jet Flow: Basic Equations and Verification for the Antarctic Circumpolar Current. IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS. 2019 Сент. 1;55(5):412-422. https://doi.org/10.1134/S0001433819050074

Author

Gnevyshev, V. G. ; Frolova, A. V. ; Kubryakov, A. A. ; Sobko, Yu V. ; Belonenko, T. V. / Interaction between Rossby Waves and a Jet Flow : Basic Equations and Verification for the Antarctic Circumpolar Current. в: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS. 2019 ; Том 55, № 5. стр. 412-422.

BibTeX

@article{a686d58032e642e5a4ee73813eeed601,
title = "Interaction between Rossby Waves and a Jet Flow: Basic Equations and Verification for the Antarctic Circumpolar Current",
abstract = "Abstract—The article focuses on the interaction of Rossby waves in the ocean with zonal jet flows. A new approach is proposed to show that nonlinearity in the long-wave approximation exactly compensates the Doppler shift. A new dispersion relation for the Rossby waves interacting with the jets is deduced from the nonlinear theory. The conclusion is verified using satellite altimetry data of the Antarctic Circumpolar Current (ACC). For the ACC area, we compare empirical velocities obtained from the altimetry data with theoretical phase velocities of Rossby waves calculated from nonlinear dispersion relation using the equivalent beta effect. The comparison shows that the new dispersion relation based on the nonlinear approach is capable of describing both the westward and the eastward propagation of mesoscale eddies in the field of sea level anomalies that can be identified as manifestation of Rossby waves in the ocean.",
keywords = "altimetry, Antarctic Circumpolar Current, dispersion relation, jet current, mesoscale eddies, nonlinear theory, Rossby waves",
author = "Gnevyshev, {V. G.} and Frolova, {A. V.} and Kubryakov, {A. A.} and Sobko, {Yu V.} and Belonenko, {T. V.}",
note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",
year = "2019",
month = sep,
day = "1",
doi = "10.1134/S0001433819050074",
language = "English",
volume = "55",
pages = "412--422",
journal = "Izvestiya, Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Interaction between Rossby Waves and a Jet Flow

T2 - Basic Equations and Verification for the Antarctic Circumpolar Current

AU - Gnevyshev, V. G.

AU - Frolova, A. V.

AU - Kubryakov, A. A.

AU - Sobko, Yu V.

AU - Belonenko, T. V.

N1 - Publisher Copyright: © 2019, Pleiades Publishing, Ltd.

PY - 2019/9/1

Y1 - 2019/9/1

N2 - Abstract—The article focuses on the interaction of Rossby waves in the ocean with zonal jet flows. A new approach is proposed to show that nonlinearity in the long-wave approximation exactly compensates the Doppler shift. A new dispersion relation for the Rossby waves interacting with the jets is deduced from the nonlinear theory. The conclusion is verified using satellite altimetry data of the Antarctic Circumpolar Current (ACC). For the ACC area, we compare empirical velocities obtained from the altimetry data with theoretical phase velocities of Rossby waves calculated from nonlinear dispersion relation using the equivalent beta effect. The comparison shows that the new dispersion relation based on the nonlinear approach is capable of describing both the westward and the eastward propagation of mesoscale eddies in the field of sea level anomalies that can be identified as manifestation of Rossby waves in the ocean.

AB - Abstract—The article focuses on the interaction of Rossby waves in the ocean with zonal jet flows. A new approach is proposed to show that nonlinearity in the long-wave approximation exactly compensates the Doppler shift. A new dispersion relation for the Rossby waves interacting with the jets is deduced from the nonlinear theory. The conclusion is verified using satellite altimetry data of the Antarctic Circumpolar Current (ACC). For the ACC area, we compare empirical velocities obtained from the altimetry data with theoretical phase velocities of Rossby waves calculated from nonlinear dispersion relation using the equivalent beta effect. The comparison shows that the new dispersion relation based on the nonlinear approach is capable of describing both the westward and the eastward propagation of mesoscale eddies in the field of sea level anomalies that can be identified as manifestation of Rossby waves in the ocean.

KW - altimetry

KW - Antarctic Circumpolar Current

KW - dispersion relation

KW - jet current

KW - mesoscale eddies

KW - nonlinear theory

KW - Rossby waves

UR - https://link.springer.com/article/10.1134/S0001433819050074

UR - http://www.scopus.com/inward/record.url?scp=85073671248&partnerID=8YFLogxK

U2 - 10.1134/S0001433819050074

DO - 10.1134/S0001433819050074

M3 - Article

AN - SCOPUS:85073671248

VL - 55

SP - 412

EP - 422

JO - Izvestiya, Atmospheric and Oceanic Physics

JF - Izvestiya, Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 5

ER -

ID: 47802700