Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex

The Lofoten Vortex (LV) is a quasi-permanent anticyclonic eddy with the characteristic of periodic regeneration in the Lofoten Basin (LB), which is one of the major areas of deep vertical mixing in the Nordic Sea. Our analysis of the LV contributes to our understanding of the variations in convectiv...

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Published in:Remote Sensing
Main Authors: Yu Liu, Jing Meng, Jianhui Wang, Guoqing Han, Xiayan Lin, Junming Chen, Qiyan Ji
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15071903
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/7/1903/ 2023-08-20T04:07:52+02:00 Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex Yu Liu Jing Meng Jianhui Wang Guoqing Han Xiayan Lin Junming Chen Qiyan Ji agris 2023-04-02 application/pdf https://doi.org/10.3390/rs15071903 EN eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs15071903 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 7; Pages: 1903 the Lofoten Vortex Argo profiles sea surface temperature vertical mixing Text 2023 ftmdpi https://doi.org/10.3390/rs15071903 2023-08-01T09:32:25Z The Lofoten Vortex (LV) is a quasi-permanent anticyclonic eddy with the characteristic of periodic regeneration in the Lofoten Basin (LB), which is one of the major areas of deep vertical mixing in the Nordic Sea. Our analysis of the LV contributes to our understanding of the variations in convective mixing in the LB. Based on drifter data and satellite altimeter data, the climatological results show that the LV has the sea surface characteristics of relative stability in terms of its spatial position and significant seasonal variations in its physical characteristics. Combined with the temperature and salinity data of Argo profiles, the vertical structures of the LV are presented here in terms of their spatial distribution and monthly variations. The wavelet analysis of the satellite sea surface temperature (SST) data shows that the period of SST anomaly (SSTA) in the LV sea area is 8–16 years. In the stage marked by a decreasing (increasing) trend of SSTA, the vertical mixing is strengthened (weakened). Current vertical mixing is clearly revealed by the Argo profiles, and the SSTA shows a significant impact of cooling. However, against a background of warming and freshening, this vertical mixing will be greatly weakened in the next increasing trending stage of the SSTA. Text Lofoten Nordic Sea MDPI Open Access Publishing Lofoten Lofoten Basin ENVELOPE(4.000,4.000,70.000,70.000) Remote Sensing 15 7 1903
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic the Lofoten Vortex
Argo profiles
sea surface temperature
vertical mixing
spellingShingle the Lofoten Vortex
Argo profiles
sea surface temperature
vertical mixing
Yu Liu
Jing Meng
Jianhui Wang
Guoqing Han
Xiayan Lin
Junming Chen
Qiyan Ji
Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
topic_facet the Lofoten Vortex
Argo profiles
sea surface temperature
vertical mixing
description The Lofoten Vortex (LV) is a quasi-permanent anticyclonic eddy with the characteristic of periodic regeneration in the Lofoten Basin (LB), which is one of the major areas of deep vertical mixing in the Nordic Sea. Our analysis of the LV contributes to our understanding of the variations in convective mixing in the LB. Based on drifter data and satellite altimeter data, the climatological results show that the LV has the sea surface characteristics of relative stability in terms of its spatial position and significant seasonal variations in its physical characteristics. Combined with the temperature and salinity data of Argo profiles, the vertical structures of the LV are presented here in terms of their spatial distribution and monthly variations. The wavelet analysis of the satellite sea surface temperature (SST) data shows that the period of SST anomaly (SSTA) in the LV sea area is 8–16 years. In the stage marked by a decreasing (increasing) trend of SSTA, the vertical mixing is strengthened (weakened). Current vertical mixing is clearly revealed by the Argo profiles, and the SSTA shows a significant impact of cooling. However, against a background of warming and freshening, this vertical mixing will be greatly weakened in the next increasing trending stage of the SSTA.
format Text
author Yu Liu
Jing Meng
Jianhui Wang
Guoqing Han
Xiayan Lin
Junming Chen
Qiyan Ji
author_facet Yu Liu
Jing Meng
Jianhui Wang
Guoqing Han
Xiayan Lin
Junming Chen
Qiyan Ji
author_sort Yu Liu
title Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
title_short Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
title_full Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
title_fullStr Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
title_full_unstemmed Analysis of Seasonal and Long-Term Variations in the Surface and Vertical Structures of the Lofoten Vortex
title_sort analysis of seasonal and long-term variations in the surface and vertical structures of the lofoten vortex
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15071903
op_coverage agris
long_lat ENVELOPE(4.000,4.000,70.000,70.000)
geographic Lofoten
Lofoten Basin
geographic_facet Lofoten
Lofoten Basin
genre Lofoten
Nordic Sea
genre_facet Lofoten
Nordic Sea
op_source Remote Sensing; Volume 15; Issue 7; Pages: 1903
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs15071903
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15071903
container_title Remote Sensing
container_volume 15
container_issue 7
container_start_page 1903
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