Standard

Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model. / Belonenko, T. V.; Volkov, D. L.; Koldunov, A. V.

в: Oceanology, Том 58, № 6, 01.11.2018, стр. 778-785.

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

Harvard

Belonenko, TV, Volkov, DL & Koldunov, AV 2018, 'Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model', Oceanology, Том. 58, № 6, стр. 778-785. https://doi.org/10.1134/S0001437018060024

APA

Belonenko, T. V., Volkov, D. L., & Koldunov, A. V. (2018). Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model. Oceanology, 58(6), 778-785. https://doi.org/10.1134/S0001437018060024

Vancouver

Belonenko TV, Volkov DL, Koldunov AV. Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model. Oceanology. 2018 Нояб. 1;58(6):778-785. https://doi.org/10.1134/S0001437018060024

Author

Belonenko, T. V. ; Volkov, D. L. ; Koldunov, A. V. / Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model. в: Oceanology. 2018 ; Том 58, № 6. стр. 778-785.

BibTeX

@article{c16a4ce68be94745b78072c1551e9dd1,
title = "Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model",
abstract = "Abstract—: The article examines low-frequency oscillations of sea level over the Beaufort Sea shelf simulated in a high-resolution regional configuration of the Massachusetts Institute of Technology general circulation model during 2007–2009 time interval. Using wavelet analysis, we obtained the spatiotemporal characteristics of shelf waves. Dispersion analysis revealed that these are freely propagating shelf waves, which represent one of the relaxation mechanisms of the Beaufort Sea water system, disturbed from a state of equilibrium by external forces, e.g., wind, upwelling, or atmospheric pressure gradients. These waves have periods of 7, 15, 27, and 75 days; wavelengths of 1510, 1300, 1400, and 550 km; and phase speeds of 2.5, 1.0, 0.6, 0.25, and 0.08 m/s. It is demonstrated that these waves can be generated by wind action north of Cape Barrow, whereupon they propagate eastward along the shelf.",
author = "Belonenko, {T. V.} and Volkov, {D. L.} and Koldunov, {A. V.}",
note = "Publisher Copyright: {\textcopyright} 2018, Pleiades Publishing, Inc.",
year = "2018",
month = nov,
day = "1",
doi = "10.1134/S0001437018060024",
language = "English",
volume = "58",
pages = "778--785",
journal = "Oceanology",
issn = "0001-4370",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Shelf Waves in the Beaufort Sea in a High-Resolution Ocean Model

AU - Belonenko, T. V.

AU - Volkov, D. L.

AU - Koldunov, A. V.

N1 - Publisher Copyright: © 2018, Pleiades Publishing, Inc.

PY - 2018/11/1

Y1 - 2018/11/1

N2 - Abstract—: The article examines low-frequency oscillations of sea level over the Beaufort Sea shelf simulated in a high-resolution regional configuration of the Massachusetts Institute of Technology general circulation model during 2007–2009 time interval. Using wavelet analysis, we obtained the spatiotemporal characteristics of shelf waves. Dispersion analysis revealed that these are freely propagating shelf waves, which represent one of the relaxation mechanisms of the Beaufort Sea water system, disturbed from a state of equilibrium by external forces, e.g., wind, upwelling, or atmospheric pressure gradients. These waves have periods of 7, 15, 27, and 75 days; wavelengths of 1510, 1300, 1400, and 550 km; and phase speeds of 2.5, 1.0, 0.6, 0.25, and 0.08 m/s. It is demonstrated that these waves can be generated by wind action north of Cape Barrow, whereupon they propagate eastward along the shelf.

AB - Abstract—: The article examines low-frequency oscillations of sea level over the Beaufort Sea shelf simulated in a high-resolution regional configuration of the Massachusetts Institute of Technology general circulation model during 2007–2009 time interval. Using wavelet analysis, we obtained the spatiotemporal characteristics of shelf waves. Dispersion analysis revealed that these are freely propagating shelf waves, which represent one of the relaxation mechanisms of the Beaufort Sea water system, disturbed from a state of equilibrium by external forces, e.g., wind, upwelling, or atmospheric pressure gradients. These waves have periods of 7, 15, 27, and 75 days; wavelengths of 1510, 1300, 1400, and 550 km; and phase speeds of 2.5, 1.0, 0.6, 0.25, and 0.08 m/s. It is demonstrated that these waves can be generated by wind action north of Cape Barrow, whereupon they propagate eastward along the shelf.

UR - http://www.scopus.com/inward/record.url?scp=85062621981&partnerID=8YFLogxK

U2 - 10.1134/S0001437018060024

DO - 10.1134/S0001437018060024

M3 - Article

AN - SCOPUS:85062621981

VL - 58

SP - 778

EP - 785

JO - Oceanology

JF - Oceanology

SN - 0001-4370

IS - 6

ER -

ID: 38435364