Research output: Contribution to journal › Article › peer-review
СЕЗОННАЯ ИЗМЕНЧИВОСТЬ ТЕРМОХАЛИННОЙ СТРУКТУРЫ МЕЗОМАСШТАБНЫХ ВИХРЕЙ В РЕГИОНЕ ЛОФОТЕНСКОЙ КОТЛОВИНЫ. / Сандалюк, Н. В.; Белоненко, Т. В.
In: ФУНДАМЕНТАЛЬНАЯ И ПРИКЛАДНАЯ ГИДРОФИЗИКА, Vol. 14, No. 1, 2021, p. 15-30.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - СЕЗОННАЯ ИЗМЕНЧИВОСТЬ ТЕРМОХАЛИННОЙ СТРУКТУРЫ МЕЗОМАСШТАБНЫХ ВИХРЕЙ В РЕГИОНЕ ЛОФОТЕНСКОЙ КОТЛОВИНЫ
AU - Сандалюк, Н. В.
AU - Белоненко, Т. В.
N1 - Publisher Copyright: © 2021 Russian Academy of Sciences,Department of the Earth Sciences. All rights reserved.
PY - 2021
Y1 - 2021
N2 - In this research, we apply the method of colocalization of altimetry data and CTD profiles from multiple platforms (research vessels, autonomous profiling floats, and gliders) to study the seasonal variability of thermohaline structures of cyclonic and anticyclonic eddies in the Lofoten Basin. We demonstrate the thermohaline structure of anticyclonic eddies reveals significant seasonal variability manifesting itself in the deepening of positive anomalies in the summer period and decreasing the vertical extension of the eddy cores. We show that a prominent feature of the thermohaline structure of cyclonic eddies is the positive salinity anomalies in the upper layer. We establish mean zonal eddy-induced transport is generally westward in both summer and winter periods. The pronounced seasonal cycle manifests itself in the intensification of zonal and meridional eddy-induced transport in winter.
AB - In this research, we apply the method of colocalization of altimetry data and CTD profiles from multiple platforms (research vessels, autonomous profiling floats, and gliders) to study the seasonal variability of thermohaline structures of cyclonic and anticyclonic eddies in the Lofoten Basin. We demonstrate the thermohaline structure of anticyclonic eddies reveals significant seasonal variability manifesting itself in the deepening of positive anomalies in the summer period and decreasing the vertical extension of the eddy cores. We show that a prominent feature of the thermohaline structure of cyclonic eddies is the positive salinity anomalies in the upper layer. We establish mean zonal eddy-induced transport is generally westward in both summer and winter periods. The pronounced seasonal cycle manifests itself in the intensification of zonal and meridional eddy-induced transport in winter.
KW - Lofoten Basin
KW - Mesoscale eddies
KW - Nordic Seas
KW - Norwegian Sea
KW - Satellite altimetry
UR - http://www.scopus.com/inward/record.url?scp=85114958204&partnerID=8YFLogxK
UR - https://www.mendeley.com/catalogue/1b229345-fe1f-336d-805f-d613915238d7/
U2 - 10.7868/s2073667321010020
DO - 10.7868/s2073667321010020
M3 - статья
AN - SCOPUS:85114958204
VL - 14
SP - 15
EP - 30
JO - ФУНДАМЕНТАЛЬНАЯ И ПРИКЛАДНАЯ ГИДРОФИЗИКА
JF - ФУНДАМЕНТАЛЬНАЯ И ПРИКЛАДНАЯ ГИДРОФИЗИКА
SN - 2073-6673
IS - 1
ER -
ID: 85982221