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Internal wave bore in the shelf zone of the sea. / Liapidevskii, V. Yu; Novotryasov, V. V.; Khrapchenkov, F. F. et al.

In: Journal of Applied Mechanics and Technical Physics, Vol. 58, No. 5, 01.09.2017, p. 809-818.

Research output: Contribution to journal › Article › peer-review

Harvard

Liapidevskii, VY, Novotryasov, VV, Khrapchenkov, FF & Yaroshchuk, IO 2017, 'Internal wave bore in the shelf zone of the sea', Journal of Applied Mechanics and Technical Physics, vol. 58, no. 5, pp. 809-818. https://doi.org/10.1134/S0021894417050066

APA

Liapidevskii, V. Y., Novotryasov, V. V., Khrapchenkov, F. F., & Yaroshchuk, I. O. (2017). Internal wave bore in the shelf zone of the sea. Journal of Applied Mechanics and Technical Physics, 58(5), 809-818. https://doi.org/10.1134/S0021894417050066

Vancouver

Liapidevskii VY, Novotryasov VV, Khrapchenkov FF, Yaroshchuk IO. Internal wave bore in the shelf zone of the sea. Journal of Applied Mechanics and Technical Physics. 2017 Sept 1;58(5):809-818. doi: 10.1134/S0021894417050066

Author

Liapidevskii, V. Yu ; Novotryasov, V. V. ; Khrapchenkov, F. F. et al. / Internal wave bore in the shelf zone of the sea. In: Journal of Applied Mechanics and Technical Physics. 2017 ; Vol. 58, No. 5. pp. 809-818.

BibTeX

@article{6fb997b5f2d5428484f90495ba098fb0,
title = "Internal wave bore in the shelf zone of the sea",
abstract = "This paper presents the observation results for the internal wave bore in the coastal region of the Sea of Japan with the use of vertical thermistor chains. The data obtained is interpreted by the mathematical models of shallow water in which the effect of nonlinearity and dispersion on the propagation of internal wave trains is taken into account. Within the framework of the theory of multilayer shallow water, the problem of transformation of a solitary wave into an internal bore is solved, and the possibility of recovery of a space-time picture of the flow during the passage of an internal bore in the section between adjacent experimental bottom stations is demonstrated.",
keywords = "internal bore, shelf zone, solitary waves, stratified flows, three-layer shallow water",
author = "Liapidevskii, {V. Yu} and Novotryasov, {V. V.} and Khrapchenkov, {F. F.} and Yaroshchuk, {I. O.}",
year = "2017",
month = sep,
day = "1",
doi = "10.1134/S0021894417050066",
language = "English",
volume = "58",
pages = "809--818",
journal = "Journal of Applied Mechanics and Technical Physics",
issn = "0021-8944",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "5",

}

RIS

TY - JOUR

T1 - Internal wave bore in the shelf zone of the sea

AU - Liapidevskii, V. Yu

AU - Novotryasov, V. V.

AU - Khrapchenkov, F. F.

AU - Yaroshchuk, I. O.

PY - 2017/9/1

Y1 - 2017/9/1

N2 - This paper presents the observation results for the internal wave bore in the coastal region of the Sea of Japan with the use of vertical thermistor chains. The data obtained is interpreted by the mathematical models of shallow water in which the effect of nonlinearity and dispersion on the propagation of internal wave trains is taken into account. Within the framework of the theory of multilayer shallow water, the problem of transformation of a solitary wave into an internal bore is solved, and the possibility of recovery of a space-time picture of the flow during the passage of an internal bore in the section between adjacent experimental bottom stations is demonstrated.

AB - This paper presents the observation results for the internal wave bore in the coastal region of the Sea of Japan with the use of vertical thermistor chains. The data obtained is interpreted by the mathematical models of shallow water in which the effect of nonlinearity and dispersion on the propagation of internal wave trains is taken into account. Within the framework of the theory of multilayer shallow water, the problem of transformation of a solitary wave into an internal bore is solved, and the possibility of recovery of a space-time picture of the flow during the passage of an internal bore in the section between adjacent experimental bottom stations is demonstrated.

KW - internal bore

KW - shelf zone

KW - solitary waves

KW - stratified flows

KW - three-layer shallow water

UR - http://www.scopus.com/inward/record.url?scp=85037528640&partnerID=8YFLogxK

U2 - 10.1134/S0021894417050066

DO - 10.1134/S0021894417050066

M3 - Article

AN - SCOPUS:85037528640

VL - 58

SP - 809

EP - 818

JO - Journal of Applied Mechanics and Technical Physics

JF - Journal of Applied Mechanics and Technical Physics

SN - 0021-8944

IS - 5

ER -

ID: 9646845