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Topographic experiments over dynamical processes in the Norwegian Sea. / Belonenko, Tatyana V.; Travkin, Vladimir S.; Koldunov, Aleksey V.; Volkov, Denis L.

в: Russian Journal of Earth Sciences, Том 21, № 1, ES1006, 16.02.2021.

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

Harvard

Belonenko, TV, Travkin, VS, Koldunov, AV & Volkov, DL 2021, 'Topographic experiments over dynamical processes in the Norwegian Sea', Russian Journal of Earth Sciences, Том. 21, № 1, ES1006. https://doi.org/10.2205/2020ES000747

APA

Belonenko, T. V., Travkin, V. S., Koldunov, A. V., & Volkov, D. L. (2021). Topographic experiments over dynamical processes in the Norwegian Sea. Russian Journal of Earth Sciences, 21(1), [ES1006]. https://doi.org/10.2205/2020ES000747

Vancouver

Belonenko TV, Travkin VS, Koldunov AV, Volkov DL. Topographic experiments over dynamical processes in the Norwegian Sea. Russian Journal of Earth Sciences. 2021 Февр. 16;21(1). ES1006. https://doi.org/10.2205/2020ES000747

Author

Belonenko, Tatyana V. ; Travkin, Vladimir S. ; Koldunov, Aleksey V. ; Volkov, Denis L. / Topographic experiments over dynamical processes in the Norwegian Sea. в: Russian Journal of Earth Sciences. 2021 ; Том 21, № 1.

BibTeX

@article{0970dbf978ef483d8f62d1169da669a2,
title = "Topographic experiments over dynamical processes in the Norwegian Sea",
abstract = "The Norwegian Atlantic Current is significantly steered by large topographic features of the Norwegian Sea. The geometry of topographic features in the region is highly variable, but the influence of this variation on the formation of a quasi-permanent anticyclonic vortex located in the center of the Lofoten Basin (Lofoten Vortex) is poorly understood. Four sensitivity experiments with a regional configuration of the Massachusetts Institute of Technology general circulation model have been carried out with an objective to investigate the role of bottom topography on the formation of the Lofoten Vortex in the Norwegian Sea. We find that the bottom topography and especially the geometry of subsurface ridges are critical for the dynamics of the Norwegian Sea and stability of the Lofoten Vortex. KEYWORDS: Norwegian Sea; Lofoten Basin; Norwegian Basin; bottom topography; MITgcm; topography experiments.",
keywords = "Norwegian Sea, Lofoten Basin, Norwegian Basin, bottom topography, MITgcm, topography experiments, LOFOTEN BASIN, NORDIC SEAS, BAROCLINIC INSTABILITY, SURFACE CIRCULATION, VERTICAL VELOCITY, DEEP CONVECTION, VORTEX, OCEAN, MODEL, STABILITY",
author = "Belonenko, {Tatyana V.} and Travkin, {Vladimir S.} and Koldunov, {Aleksey V.} and Volkov, {Denis L.}",
note = "Publisher Copyright: Copyright {\textcopyright} 2021 by the Geophysical Center RAS.",
year = "2021",
month = feb,
day = "16",
doi = "10.2205/2020ES000747",
language = "English",
volume = "21",
journal = "Russian Journal of Earth Sciences",
issn = "1681-1178",
publisher = "American Geophysical Union",
number = "1",

}

RIS

TY - JOUR

T1 - Topographic experiments over dynamical processes in the Norwegian Sea

AU - Belonenko, Tatyana V.

AU - Travkin, Vladimir S.

AU - Koldunov, Aleksey V.

AU - Volkov, Denis L.

N1 - Publisher Copyright: Copyright © 2021 by the Geophysical Center RAS.

PY - 2021/2/16

Y1 - 2021/2/16

N2 - The Norwegian Atlantic Current is significantly steered by large topographic features of the Norwegian Sea. The geometry of topographic features in the region is highly variable, but the influence of this variation on the formation of a quasi-permanent anticyclonic vortex located in the center of the Lofoten Basin (Lofoten Vortex) is poorly understood. Four sensitivity experiments with a regional configuration of the Massachusetts Institute of Technology general circulation model have been carried out with an objective to investigate the role of bottom topography on the formation of the Lofoten Vortex in the Norwegian Sea. We find that the bottom topography and especially the geometry of subsurface ridges are critical for the dynamics of the Norwegian Sea and stability of the Lofoten Vortex. KEYWORDS: Norwegian Sea; Lofoten Basin; Norwegian Basin; bottom topography; MITgcm; topography experiments.

AB - The Norwegian Atlantic Current is significantly steered by large topographic features of the Norwegian Sea. The geometry of topographic features in the region is highly variable, but the influence of this variation on the formation of a quasi-permanent anticyclonic vortex located in the center of the Lofoten Basin (Lofoten Vortex) is poorly understood. Four sensitivity experiments with a regional configuration of the Massachusetts Institute of Technology general circulation model have been carried out with an objective to investigate the role of bottom topography on the formation of the Lofoten Vortex in the Norwegian Sea. We find that the bottom topography and especially the geometry of subsurface ridges are critical for the dynamics of the Norwegian Sea and stability of the Lofoten Vortex. KEYWORDS: Norwegian Sea; Lofoten Basin; Norwegian Basin; bottom topography; MITgcm; topography experiments.

KW - Norwegian Sea

KW - Lofoten Basin

KW - Norwegian Basin

KW - bottom topography

KW - MITgcm

KW - topography experiments

KW - LOFOTEN BASIN

KW - NORDIC SEAS

KW - BAROCLINIC INSTABILITY

KW - SURFACE CIRCULATION

KW - VERTICAL VELOCITY

KW - DEEP CONVECTION

KW - VORTEX

KW - OCEAN

KW - MODEL

KW - STABILITY

UR - http://www.scopus.com/inward/record.url?scp=85102683362&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/f4a1bba4-d629-33ea-bff3-bfaab31f463b/

U2 - 10.2205/2020ES000747

DO - 10.2205/2020ES000747

M3 - Article

AN - SCOPUS:85102683362

VL - 21

JO - Russian Journal of Earth Sciences

JF - Russian Journal of Earth Sciences

SN - 1681-1178

IS - 1

M1 - ES1006

ER -

ID: 75066184