Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll

The Southern Ocean front (SOF) is an important factor that affects the heat exchange and material transport of the Southern Ocean. In the past two decades, with the advancements in satellite remote-sensing technology, the study of the spatio-temporal variability of the Southern Ocean front has becom...

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Autores principales: Zhi Wang, Ge Chen, Yong Han, Chunyong Ma, Ming Lv
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/776d2ea1fe9f461f896cad576ee6e8a5
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spelling oai:doaj.org-article:776d2ea1fe9f461f896cad576ee6e8a52021-11-11T18:55:35ZSouthwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll10.3390/rs132144022072-4292https://doaj.org/article/776d2ea1fe9f461f896cad576ee6e8a52021-11-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4402https://doaj.org/toc/2072-4292The Southern Ocean front (SOF) is an important factor that affects the heat exchange and material transport of the Southern Ocean. In the past two decades, with the advancements in satellite remote-sensing technology, the study of the spatio-temporal variability of the Southern Ocean front has become a new hot topic. Nevertheless, the southwestern Atlantic, as an important part of the Southern Ocean, is poorly studied in this regard. Based on the 16-year (2004–2019) high-resolution satellite observations of sea surface temperature (SST) and 13-year (2007–2019) observations of chlorophyll (CHL), this study detected and analyzed the position and seasonal variation of the SOF in the southwestern Atlantic using a gradient-based frontal detection method. According to the experimental results, the thermal front (derived from the SST data) disappeared in winter due to the spatially uniform surface cooling, whereas the ocean color front (derived from the CHL data) existed without remarkable spatio-temporal changes. Furthermore, the exact position and seasonal variation of the SOF in the southwestern Atlantic are determined by comparing the paths of the two fronts. Since the formation of the Kuroshio front in the East China Sea (ECS) is similar to the SOF in the southwestern Atlantic, the seasonal distributions of the two fronts were compared. Apart from that, the Kuroshio thermal fronts were mostly distributed in winter and less in summer, while the Southern Ocean thermal fronts showed the opposite. These results indicated that the ocean current properties significantly influence the spatio-temporal variability of the front.Zhi WangGe ChenYong HanChunyong MaMing LvMDPI AGarticleSouthern Ocean frontsouthwestern Atlanticsea surface temperaturechlorophyllScienceQENRemote Sensing, Vol 13, Iss 4402, p 4402 (2021)
institution DOAJ
collection DOAJ
language EN
topic Southern Ocean front
southwestern Atlantic
sea surface temperature
chlorophyll
Science
Q
spellingShingle Southern Ocean front
southwestern Atlantic
sea surface temperature
chlorophyll
Science
Q
Zhi Wang
Ge Chen
Yong Han
Chunyong Ma
Ming Lv
Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
description The Southern Ocean front (SOF) is an important factor that affects the heat exchange and material transport of the Southern Ocean. In the past two decades, with the advancements in satellite remote-sensing technology, the study of the spatio-temporal variability of the Southern Ocean front has become a new hot topic. Nevertheless, the southwestern Atlantic, as an important part of the Southern Ocean, is poorly studied in this regard. Based on the 16-year (2004–2019) high-resolution satellite observations of sea surface temperature (SST) and 13-year (2007–2019) observations of chlorophyll (CHL), this study detected and analyzed the position and seasonal variation of the SOF in the southwestern Atlantic using a gradient-based frontal detection method. According to the experimental results, the thermal front (derived from the SST data) disappeared in winter due to the spatially uniform surface cooling, whereas the ocean color front (derived from the CHL data) existed without remarkable spatio-temporal changes. Furthermore, the exact position and seasonal variation of the SOF in the southwestern Atlantic are determined by comparing the paths of the two fronts. Since the formation of the Kuroshio front in the East China Sea (ECS) is similar to the SOF in the southwestern Atlantic, the seasonal distributions of the two fronts were compared. Apart from that, the Kuroshio thermal fronts were mostly distributed in winter and less in summer, while the Southern Ocean thermal fronts showed the opposite. These results indicated that the ocean current properties significantly influence the spatio-temporal variability of the front.
format article
author Zhi Wang
Ge Chen
Yong Han
Chunyong Ma
Ming Lv
author_facet Zhi Wang
Ge Chen
Yong Han
Chunyong Ma
Ming Lv
author_sort Zhi Wang
title Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
title_short Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
title_full Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
title_fullStr Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
title_full_unstemmed Southwestern Atlantic Ocean Fronts Detected from Satellite-Derived SST and Chlorophyll
title_sort southwestern atlantic ocean fronts detected from satellite-derived sst and chlorophyll
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/776d2ea1fe9f461f896cad576ee6e8a5
work_keys_str_mv AT zhiwang southwesternatlanticoceanfrontsdetectedfromsatellitederivedsstandchlorophyll
AT gechen southwesternatlanticoceanfrontsdetectedfromsatellitederivedsstandchlorophyll
AT yonghan southwesternatlanticoceanfrontsdetectedfromsatellitederivedsstandchlorophyll
AT chunyongma southwesternatlanticoceanfrontsdetectedfromsatellitederivedsstandchlorophyll
AT minglv southwesternatlanticoceanfrontsdetectedfromsatellitederivedsstandchlorophyll
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