Standard

"Hollow" Waves in the Lofoten Basin of the Norwegian Sea. / Belonenko, T.V.; Volkov, D.L.; Foux, V.R.

Fluxes and Structures in Fluids. МАКС Пресс, 2013. стр. 31-34.

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › научная

Harvard

Belonenko, TV, Volkov, DL & Foux, VR 2013, "Hollow" Waves in the Lofoten Basin of the Norwegian Sea. в Fluxes and Structures in Fluids. МАКС Пресс, стр. 31-34.

APA

Belonenko, T. V., Volkov, D. L., & Foux, V. R. (2013). "Hollow" Waves in the Lofoten Basin of the Norwegian Sea. в Fluxes and Structures in Fluids (стр. 31-34). МАКС Пресс.

Vancouver

Belonenko TV, Volkov DL, Foux VR. "Hollow" Waves in the Lofoten Basin of the Norwegian Sea. в Fluxes and Structures in Fluids. МАКС Пресс. 2013. стр. 31-34

Author

Belonenko, T.V. ; Volkov, D.L. ; Foux, V.R. / "Hollow" Waves in the Lofoten Basin of the Norwegian Sea. Fluxes and Structures in Fluids. МАКС Пресс, 2013. стр. 31-34

BibTeX

@inproceedings{fd9ea2976d1a4869afc57d18b38f9288,
title = "{"}Hollow{"} Waves in the Lofoten Basin of the Norwegian Sea.",
abstract = "A sub-Arctic {"}hot spot{"} of intense synoptic-scale variability is observed in the Lofoten Basin (LB) of the Norwegian Sea. Using ERS-1/2 and Envisat satellite altimetry measurements, we discover a cyclonic propagation of the synoptic-scale sea surface height anomalies around the center of the LB. Surface drifter trajectories do not reveal an associated coherent near-surface cyclonic flow suggesting that the propagating signals have a wavelike nature. We identify a dipole and a quadrupole wave modes rotating around the center of the LB, obtain analytic dispersion relations for these modes, and demonstrate that the observed propagation is a manifestation of topographic Rossby waves. Most of the observed waves have a wavelength of about 500 km and phase speeds ranging from 2 to 10 km/day. We show that these waves are largely responsible for the localization and amplification of sea surface height variability in the center of the LB.",
keywords = "{"}Hollow{"} Waves, the Lofoten Basin, Norwegian Sea, волны, вихри",
author = "T.V. Belonenko and D.L. Volkov and V.R. Foux",
year = "2013",
language = "English",
isbn = "978-5-317-04468-8",
pages = "31--34",
booktitle = "Fluxes and Structures in Fluids",
publisher = "МАКС Пресс",
address = "Russian Federation",

}

RIS

TY - GEN

T1 - "Hollow" Waves in the Lofoten Basin of the Norwegian Sea.

AU - Belonenko, T.V.

AU - Volkov, D.L.

AU - Foux, V.R.

PY - 2013

Y1 - 2013

N2 - A sub-Arctic "hot spot" of intense synoptic-scale variability is observed in the Lofoten Basin (LB) of the Norwegian Sea. Using ERS-1/2 and Envisat satellite altimetry measurements, we discover a cyclonic propagation of the synoptic-scale sea surface height anomalies around the center of the LB. Surface drifter trajectories do not reveal an associated coherent near-surface cyclonic flow suggesting that the propagating signals have a wavelike nature. We identify a dipole and a quadrupole wave modes rotating around the center of the LB, obtain analytic dispersion relations for these modes, and demonstrate that the observed propagation is a manifestation of topographic Rossby waves. Most of the observed waves have a wavelength of about 500 km and phase speeds ranging from 2 to 10 km/day. We show that these waves are largely responsible for the localization and amplification of sea surface height variability in the center of the LB.

AB - A sub-Arctic "hot spot" of intense synoptic-scale variability is observed in the Lofoten Basin (LB) of the Norwegian Sea. Using ERS-1/2 and Envisat satellite altimetry measurements, we discover a cyclonic propagation of the synoptic-scale sea surface height anomalies around the center of the LB. Surface drifter trajectories do not reveal an associated coherent near-surface cyclonic flow suggesting that the propagating signals have a wavelike nature. We identify a dipole and a quadrupole wave modes rotating around the center of the LB, obtain analytic dispersion relations for these modes, and demonstrate that the observed propagation is a manifestation of topographic Rossby waves. Most of the observed waves have a wavelength of about 500 km and phase speeds ranging from 2 to 10 km/day. We show that these waves are largely responsible for the localization and amplification of sea surface height variability in the center of the LB.

KW - "Hollow" Waves

KW - the Lofoten Basin

KW - Norwegian Sea

KW - волны

KW - вихри

UR - https://search.rsl.ru/ru/search#q=9785317044688

M3 - Conference contribution

SN - 978-5-317-04468-8

SP - 31

EP - 34

BT - Fluxes and Structures in Fluids

PB - МАКС Пресс

ER -

ID: 4621790