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Nonlinear waves in marginally stable flows of Antarctic Bottom Water. / Makarenko, N. I.; Maltseva, J. L.; Morozov, E. G. et al.

In: IOP Conference Series: Earth and Environmental Science, Vol. 193, No. 1, 012041, 30.10.2018.

Research output: Contribution to journal › Conference article › peer-review

Harvard

Makarenko, NI, Maltseva, JL, Morozov, EG, Tarakanov, RY & Ivanova, KA 2018, 'Nonlinear waves in marginally stable flows of Antarctic Bottom Water', IOP Conference Series: Earth and Environmental Science, vol. 193, no. 1, 012041. https://doi.org/10.1088/1755-1315/193/1/012041

APA

Makarenko, N. I., Maltseva, J. L., Morozov, E. G., Tarakanov, R. Y., & Ivanova, K. A. (2018). Nonlinear waves in marginally stable flows of Antarctic Bottom Water. IOP Conference Series: Earth and Environmental Science, 193(1), [012041]. https://doi.org/10.1088/1755-1315/193/1/012041

Vancouver

Makarenko NI, Maltseva JL, Morozov EG, Tarakanov RY, Ivanova KA. Nonlinear waves in marginally stable flows of Antarctic Bottom Water. IOP Conference Series: Earth and Environmental Science. 2018 Oct 30;193(1):012041. doi: 10.1088/1755-1315/193/1/012041

Author

Makarenko, N. I. ; Maltseva, J. L. ; Morozov, E. G. et al. / Nonlinear waves in marginally stable flows of Antarctic Bottom Water. In: IOP Conference Series: Earth and Environmental Science. 2018 ; Vol. 193, No. 1.

BibTeX

@article{fd946d42dc5741e3a3c73f7f1e31d379,
title = "Nonlinear waves in marginally stable flows of Antarctic Bottom Water",
abstract = "In this paper, we study internal waves and stratified flows in the Romanche Fracture Zone of the Mid Atlantic Ridge. Theoretical analysis involves mathematical formulation of stratified flows which uses LADCP- and CTD-data obtained from field observation in the cruises of RV Akademik Sergey Vavilov. We discuss the 2.5-layer model of the fluid with exponential stratification of both layers. The long-wave approximate model describing travelling waves is constructed by means of scaling procedure with a small Boussinesq parameter. It is demonstrated that solitary wave regimes can be affected by the Kelvin - Helmholtz instability arising due to interfacial velocity shear in upstream flow.",
keywords = "INTERNAL WAVES",
author = "Makarenko, {N. I.} and Maltseva, {J. L.} and Morozov, {E. G.} and Tarakanov, {R. Yu} and Ivanova, {K. A.}",
year = "2018",
month = oct,
day = "30",
doi = "10.1088/1755-1315/193/1/012041",
language = "English",
volume = "193",
journal = "IOP Conference Series: Earth and Environmental Science",
issn = "1755-1307",
publisher = "IOP Publishing Ltd.",
number = "1",
note = "5th All-Russian Conference with International Participation on Polar Mechanics 2018 ; Conference date: 09-10-2018 Through 11-10-2018",

}

RIS

TY - JOUR

T1 - Nonlinear waves in marginally stable flows of Antarctic Bottom Water

AU - Makarenko, N. I.

AU - Maltseva, J. L.

AU - Morozov, E. G.

AU - Tarakanov, R. Yu

AU - Ivanova, K. A.

PY - 2018/10/30

Y1 - 2018/10/30

N2 - In this paper, we study internal waves and stratified flows in the Romanche Fracture Zone of the Mid Atlantic Ridge. Theoretical analysis involves mathematical formulation of stratified flows which uses LADCP- and CTD-data obtained from field observation in the cruises of RV Akademik Sergey Vavilov. We discuss the 2.5-layer model of the fluid with exponential stratification of both layers. The long-wave approximate model describing travelling waves is constructed by means of scaling procedure with a small Boussinesq parameter. It is demonstrated that solitary wave regimes can be affected by the Kelvin - Helmholtz instability arising due to interfacial velocity shear in upstream flow.

AB - In this paper, we study internal waves and stratified flows in the Romanche Fracture Zone of the Mid Atlantic Ridge. Theoretical analysis involves mathematical formulation of stratified flows which uses LADCP- and CTD-data obtained from field observation in the cruises of RV Akademik Sergey Vavilov. We discuss the 2.5-layer model of the fluid with exponential stratification of both layers. The long-wave approximate model describing travelling waves is constructed by means of scaling procedure with a small Boussinesq parameter. It is demonstrated that solitary wave regimes can be affected by the Kelvin - Helmholtz instability arising due to interfacial velocity shear in upstream flow.

KW - INTERNAL WAVES

UR - http://www.scopus.com/inward/record.url?scp=85056474924&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/193/1/012041

DO - 10.1088/1755-1315/193/1/012041

M3 - Conference article

AN - SCOPUS:85056474924

VL - 193

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012041

T2 - 5th All-Russian Conference with International Participation on Polar Mechanics 2018

Y2 - 9 October 2018 through 11 October 2018

ER -

ID: 17468247