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Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью. / Konik, A. A.; Kozlov, I. E.; Zimin, A. V.; Atadzhanova, O. A.

In: Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa, Vol. 17, No. 5, 2020, p. 191-201.

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

Harvard

Konik, AA, Kozlov, IE, Zimin, AV & Atadzhanova, OA 2020, 'Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью', Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa, vol. 17, no. 5, pp. 191-201. https://doi.org/10.21046/2070-7401-2020-17-5-191-201

APA

Konik, A. A., Kozlov, I. E., Zimin, A. V., & Atadzhanova, O. A. (2020). Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью. Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa, 17(5), 191-201. https://doi.org/10.21046/2070-7401-2020-17-5-191-201

Vancouver

Konik AA, Kozlov IE, Zimin AV, Atadzhanova OA. Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью. Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa. 2020;17(5):191-201. https://doi.org/10.21046/2070-7401-2020-17-5-191-201

Author

Konik, A. A. ; Kozlov, I. E. ; Zimin, A. V. ; Atadzhanova, O. A. / Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью. In: Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa. 2020 ; Vol. 17, No. 5. pp. 191-201.

BibTeX

@article{d3137ad43c334fe69a928e67eda7417f,
title = "Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью",
abstract = "In this paper, based on the analysis of satellite radar images and averaged sea surface temperature fields, we study the relationship between the eddy structures of the Barents Sea and the position of the main frontal zones in the summer of 2007 and 2009, where different ice conditions are observed. We considered the Marginal Ice frontal area and the Polar front that are characterized by horizontal temperature gradient of 0.04 °?/km and width of 75-136 km. Altogether 1135 eddies were identified in the data. It was shown that in 2009 the number of eddies observed in the boundaries of the frontal zones were twice as high as in 2007. In general, the number of eddies inside the frontal zones did not exceed 26 % in the Barents Sea, meaning that the reason for the generation of other eddies may be their generation mechanisms, probably related to inhomogeneity of the bottom relief and driving wind fields.",
keywords = "Arctic Ocean, Barents Sea, Frontal zones, Ocean eddies, Sea surface temperature, Synthetic aperture radar",
author = "Konik, {A. A.} and Kozlov, {I. E.} and Zimin, {A. V.} and Atadzhanova, {O. A.}",
note = "Publisher Copyright: {\textcopyright} 2020 Space Research Institute of the Russian Academy of Sciences. All rights reserved. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.",
year = "2020",
doi = "10.21046/2070-7401-2020-17-5-191-201",
language = "русский",
volume = "17",
pages = "191--201",
journal = "СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА",
issn = "2070-7401",
publisher = "Институт космических исследований Российской академии наук",
number = "5",

}

RIS

TY - JOUR

T1 - Спутниковые наблюдения вихрей и фронтальных зон Баренцева моря в  годы с  различной ледовитостью

AU - Konik, A. A.

AU - Kozlov, I. E.

AU - Zimin, A. V.

AU - Atadzhanova, O. A.

N1 - Publisher Copyright: © 2020 Space Research Institute of the Russian Academy of Sciences. All rights reserved. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.

PY - 2020

Y1 - 2020

N2 - In this paper, based on the analysis of satellite radar images and averaged sea surface temperature fields, we study the relationship between the eddy structures of the Barents Sea and the position of the main frontal zones in the summer of 2007 and 2009, where different ice conditions are observed. We considered the Marginal Ice frontal area and the Polar front that are characterized by horizontal temperature gradient of 0.04 °?/km and width of 75-136 km. Altogether 1135 eddies were identified in the data. It was shown that in 2009 the number of eddies observed in the boundaries of the frontal zones were twice as high as in 2007. In general, the number of eddies inside the frontal zones did not exceed 26 % in the Barents Sea, meaning that the reason for the generation of other eddies may be their generation mechanisms, probably related to inhomogeneity of the bottom relief and driving wind fields.

AB - In this paper, based on the analysis of satellite radar images and averaged sea surface temperature fields, we study the relationship between the eddy structures of the Barents Sea and the position of the main frontal zones in the summer of 2007 and 2009, where different ice conditions are observed. We considered the Marginal Ice frontal area and the Polar front that are characterized by horizontal temperature gradient of 0.04 °?/km and width of 75-136 km. Altogether 1135 eddies were identified in the data. It was shown that in 2009 the number of eddies observed in the boundaries of the frontal zones were twice as high as in 2007. In general, the number of eddies inside the frontal zones did not exceed 26 % in the Barents Sea, meaning that the reason for the generation of other eddies may be their generation mechanisms, probably related to inhomogeneity of the bottom relief and driving wind fields.

KW - Arctic Ocean

KW - Barents Sea

KW - Frontal zones

KW - Ocean eddies

KW - Sea surface temperature

KW - Synthetic aperture radar

UR - http://www.scopus.com/inward/record.url?scp=85096435535&partnerID=8YFLogxK

U2 - 10.21046/2070-7401-2020-17-5-191-201

DO - 10.21046/2070-7401-2020-17-5-191-201

M3 - статья

AN - SCOPUS:85096435535

VL - 17

SP - 191

EP - 201

JO - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА

JF - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА

SN - 2070-7401

IS - 5

ER -

ID: 73106730