Peculiarities of Formation of the Density Field in Mesoscale Eddies of the Lofoten Basin: Part 2

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Peculiarities of Formation of the Density Field in Mesoscale Eddies of the Lofoten Basin: Part 2. / Белоненко, Татьяна Васильевна ; Новоселова, Елена Владимировна; Жмур, Владимир Владимирович .

в: Oceanology, Том 62, № 3, 06.2022, стр. 289-302.

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

BibTeX

@article{3540349944a84cadb458f44f7735a878,

title = "Peculiarities of Formation of the Density Field in Mesoscale Eddies of the Lofoten Basin: Part 2",

abstract = "Abstract—: This paper continues the studies of the authors of the Brunt–V{\"a}is{\"a}l{\"a} (BV) frequency changes caused by mesoscale eddies of various polarities. In Part 1, we discussed the theoretical conclusions, whereas Part 2 provides the interpretation of these results on the basis of natural data. The studied region is the Lofoten Basin of the Norwegian Sea. The analysis considers the data of GLORYS12V1 oceanic reanalysis at June 10, 2010. Two eddies are considered: a quasi-permanent anticyclone, Lofoten eddy (LE), located in the center of the basin and a cyclone located southeast of LE. The mathematical formulas are verified, the characteristics of eddies are calculated, and the profiles and vertical sections of potential vorticity and BV frequency are studied. Combined analysis of natural and theoretical material results in indirect estimation of eddies, which cannot be directly measured and modeled.",

keywords = "Brunt–V{\"a}is{\"a}l{\"a} frequency, Lofoten Basin, buoyancy frequency, mesoscale eddies, potential vorticity",

author = "Белоненко, {Татьяна Васильевна} and Новоселова, {Елена Владимировна} and Жмур, {Владимир Владимирович}",

note = "Publisher Copyright: {\textcopyright} 2022, Pleiades Publishing, Inc.",

year = "2022",

month = jun,

doi = "10.1134/s0001437022030171",

language = "English",

volume = "62",

pages = "289--302",

journal = "Oceanology",

issn = "0001-4370",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "3",

}

RIS

TY - JOUR

T1 - Peculiarities of Formation of the Density Field in Mesoscale Eddies of the Lofoten Basin: Part 2

AU - Белоненко, Татьяна Васильевна

AU - Новоселова, Елена Владимировна

AU - Жмур, Владимир Владимирович

PY - 2022/6

Y1 - 2022/6

N2 - Abstract—: This paper continues the studies of the authors of the Brunt–Väisälä (BV) frequency changes caused by mesoscale eddies of various polarities. In Part 1, we discussed the theoretical conclusions, whereas Part 2 provides the interpretation of these results on the basis of natural data. The studied region is the Lofoten Basin of the Norwegian Sea. The analysis considers the data of GLORYS12V1 oceanic reanalysis at June 10, 2010. Two eddies are considered: a quasi-permanent anticyclone, Lofoten eddy (LE), located in the center of the basin and a cyclone located southeast of LE. The mathematical formulas are verified, the characteristics of eddies are calculated, and the profiles and vertical sections of potential vorticity and BV frequency are studied. Combined analysis of natural and theoretical material results in indirect estimation of eddies, which cannot be directly measured and modeled.

AB - Abstract—: This paper continues the studies of the authors of the Brunt–Väisälä (BV) frequency changes caused by mesoscale eddies of various polarities. In Part 1, we discussed the theoretical conclusions, whereas Part 2 provides the interpretation of these results on the basis of natural data. The studied region is the Lofoten Basin of the Norwegian Sea. The analysis considers the data of GLORYS12V1 oceanic reanalysis at June 10, 2010. Two eddies are considered: a quasi-permanent anticyclone, Lofoten eddy (LE), located in the center of the basin and a cyclone located southeast of LE. The mathematical formulas are verified, the characteristics of eddies are calculated, and the profiles and vertical sections of potential vorticity and BV frequency are studied. Combined analysis of natural and theoretical material results in indirect estimation of eddies, which cannot be directly measured and modeled.

KW - Brunt–Väisälä frequency

KW - Lofoten Basin

KW - buoyancy frequency

KW - mesoscale eddies

KW - potential vorticity

UR - http://www.scopus.com/inward/record.url?scp=85134218758&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/31340c72-2760-3c37-9c3a-b76c77b14c0e/

U2 - 10.1134/s0001437022030171

DO - 10.1134/s0001437022030171

M3 - Article

VL - 62

SP - 289

EP - 302

JO - Oceanology

JF - Oceanology

SN - 0001-4370

IS - 3

ER -

ID: 96875443