Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension

Vigorous mesoscale eddies are broadly distributed in the Kuroshio Extension and can generally be identified from sea surface height (SSH) and sea surface temperature (SST) fields. Nevertheless, the changes in SSH and SST caused by mesoscale eddies and their seasonal correlation in the Kuroshio Exten...

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Main Authors: Wei Cui, Jungang Yang, Yongjun Jia, Jie Zhang
Format: Article
Language:English
Published: MDPI AG 2022-11-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/22/5776
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author Wei Cui
Jungang Yang
Yongjun Jia
Jie Zhang
author_facet Wei Cui
Jungang Yang
Yongjun Jia
Jie Zhang
author_sort Wei Cui
collection DOAJ
description Vigorous mesoscale eddies are broadly distributed in the Kuroshio Extension and can generally be identified from sea surface height (SSH) and sea surface temperature (SST) fields. Nevertheless, the changes in SSH and SST caused by mesoscale eddies and their seasonal correlation in the Kuroshio Extension are not clear, as well as the difference between identified eddy results from the two data. Combining in situ Argo float profiles data, the correlation between SSH anomaly (SSHA) and SST anomaly (SSTA) signals in mesoscale eddies are analyzed. The result shows that SSTA–SSHA signals inside eddies are generally more correlated in winter than in summer. Argo subsurface temperature anomalies <i>θ′</i> and SSHA signals inside eddies show a high correlation, with a regression coefficient <i>θ′</i>/SSHA of about 7 °C·m<sup>−1</sup>, while correlations of Argo <i>θ′</i>–SSTA inside eddies are low. Generally, the lifetime and propagation distance of SSTA-based eddies are shorter and smaller than those of SSHA-based eddies, which may be related to the rapid changes in SSTA field and the interference of small-scale oceanic signal in the SST field. Comparing with SSHA-based eddies, which exist primarily around the region of the Kuroshio mainstream (33°–36°N), SSTA-based eddies are concentrated in the Oyashio Extension (39°–42°N), where SST gradient is large, and changes in SST fields caused by mesoscale eddies are more obvious and more likely to be captured by satellites there. In addition, the geographical distributions of SSHA- and SSTA-based eddy amplitudes are consistent with the absolute dynamic topography and SST gradient.
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spelling doaj.art-2be0aec65d4248e89cd3f5101fd7bf0e2023-11-24T09:50:16ZengMDPI AGRemote Sensing2072-42922022-11-011422577610.3390/rs14225776Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio ExtensionWei Cui0Jungang Yang1Yongjun Jia2Jie Zhang3First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaNational Satellite Ocean Application Service, Beijing 100081, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaVigorous mesoscale eddies are broadly distributed in the Kuroshio Extension and can generally be identified from sea surface height (SSH) and sea surface temperature (SST) fields. Nevertheless, the changes in SSH and SST caused by mesoscale eddies and their seasonal correlation in the Kuroshio Extension are not clear, as well as the difference between identified eddy results from the two data. Combining in situ Argo float profiles data, the correlation between SSH anomaly (SSHA) and SST anomaly (SSTA) signals in mesoscale eddies are analyzed. The result shows that SSTA–SSHA signals inside eddies are generally more correlated in winter than in summer. Argo subsurface temperature anomalies <i>θ′</i> and SSHA signals inside eddies show a high correlation, with a regression coefficient <i>θ′</i>/SSHA of about 7 °C·m<sup>−1</sup>, while correlations of Argo <i>θ′</i>–SSTA inside eddies are low. Generally, the lifetime and propagation distance of SSTA-based eddies are shorter and smaller than those of SSHA-based eddies, which may be related to the rapid changes in SSTA field and the interference of small-scale oceanic signal in the SST field. Comparing with SSHA-based eddies, which exist primarily around the region of the Kuroshio mainstream (33°–36°N), SSTA-based eddies are concentrated in the Oyashio Extension (39°–42°N), where SST gradient is large, and changes in SST fields caused by mesoscale eddies are more obvious and more likely to be captured by satellites there. In addition, the geographical distributions of SSHA- and SSTA-based eddy amplitudes are consistent with the absolute dynamic topography and SST gradient.https://www.mdpi.com/2072-4292/14/22/5776mesoscale eddysea surface heightsea surface temperatureKuroshio Extension
spellingShingle Wei Cui
Jungang Yang
Yongjun Jia
Jie Zhang
Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
Remote Sensing
mesoscale eddy
sea surface height
sea surface temperature
Kuroshio Extension
title Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
title_full Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
title_fullStr Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
title_full_unstemmed Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
title_short Oceanic Eddy Detection and Analysis from Satellite-Derived SSH and SST Fields in the Kuroshio Extension
title_sort oceanic eddy detection and analysis from satellite derived ssh and sst fields in the kuroshio extension
topic mesoscale eddy
sea surface height
sea surface temperature
Kuroshio Extension
url https://www.mdpi.com/2072-4292/14/22/5776
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AT jungangyang oceaniceddydetectionandanalysisfromsatellitederivedsshandsstfieldsinthekuroshioextension
AT yongjunjia oceaniceddydetectionandanalysisfromsatellitederivedsshandsstfieldsinthekuroshioextension
AT jiezhang oceaniceddydetectionandanalysisfromsatellitederivedsshandsstfieldsinthekuroshioextension