Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean

The ocean is filled with mesoscale eddies that account for most of the oceanic kinetic energy. The importance of eddies in transporting properties and energy across the ocean basins has led to numerous efforts to track their motion. Here, we implement a computer vision technique—the optical flow—to...

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Published in:Remote Sensing
Main Authors: Denis L. Volkov, Shahriar Negahdaripour
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15153894
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/15/3894/ 2023-09-05T13:15:20+02:00 Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean Denis L. Volkov Shahriar Negahdaripour agris 2023-08-07 application/pdf https://doi.org/10.3390/rs15153894 EN eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs15153894 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 15; Pages: 3894 mesoscale eddies eddy propagation Rossby waves optical flow computer vision sea surface height satellite altimetry South Atlantic Ocean Text 2023 ftmdpi https://doi.org/10.3390/rs15153894 2023-08-13T23:51:41Z The ocean is filled with mesoscale eddies that account for most of the oceanic kinetic energy. The importance of eddies in transporting properties and energy across the ocean basins has led to numerous efforts to track their motion. Here, we implement a computer vision technique—the optical flow—to map the pathways of mesoscale eddies in the South Atlantic Ocean. The optical flow is applied to the pairs of consecutive sea surface height maps produced from a nearly 30-year-long satellite altimetry record. In contrast to other methods to estimate the eddy propagation velocity, the optical flow can reveal the temporal evolution of eddy motion, which is particularly useful in the regions of strong currents. We present the time-dependent estimates of the speed and direction of eddy propagation in the Eulerian frame of reference. In an excellent agreement with earlier studies, the obtained pattern of eddy propagation reveals the interaction of eddies with the background flow and the bottom topography. We show that in the Antarctic Circumpolar Current, the variability of the eddy propagation velocity is correlated with the variability of the surface geostrophic velocity, demonstrating the robustness of the optical flow to detect the time-variable part of eddy motion. Text Antarc* Antarctic South Atlantic Ocean MDPI Open Access Publishing Antarctic The Antarctic Remote Sensing 15 15 3894
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic mesoscale eddies
eddy propagation
Rossby waves
optical flow
computer vision
sea surface height
satellite altimetry
South Atlantic Ocean
spellingShingle mesoscale eddies
eddy propagation
Rossby waves
optical flow
computer vision
sea surface height
satellite altimetry
South Atlantic Ocean
Denis L. Volkov
Shahriar Negahdaripour
Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
topic_facet mesoscale eddies
eddy propagation
Rossby waves
optical flow
computer vision
sea surface height
satellite altimetry
South Atlantic Ocean
description The ocean is filled with mesoscale eddies that account for most of the oceanic kinetic energy. The importance of eddies in transporting properties and energy across the ocean basins has led to numerous efforts to track their motion. Here, we implement a computer vision technique—the optical flow—to map the pathways of mesoscale eddies in the South Atlantic Ocean. The optical flow is applied to the pairs of consecutive sea surface height maps produced from a nearly 30-year-long satellite altimetry record. In contrast to other methods to estimate the eddy propagation velocity, the optical flow can reveal the temporal evolution of eddy motion, which is particularly useful in the regions of strong currents. We present the time-dependent estimates of the speed and direction of eddy propagation in the Eulerian frame of reference. In an excellent agreement with earlier studies, the obtained pattern of eddy propagation reveals the interaction of eddies with the background flow and the bottom topography. We show that in the Antarctic Circumpolar Current, the variability of the eddy propagation velocity is correlated with the variability of the surface geostrophic velocity, demonstrating the robustness of the optical flow to detect the time-variable part of eddy motion.
format Text
author Denis L. Volkov
Shahriar Negahdaripour
author_facet Denis L. Volkov
Shahriar Negahdaripour
author_sort Denis L. Volkov
title Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
title_short Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
title_full Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
title_fullStr Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
title_full_unstemmed Implementation of the Optical Flow to Estimate the Propagation of Eddies in the South Atlantic Ocean
title_sort implementation of the optical flow to estimate the propagation of eddies in the south atlantic ocean
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15153894
op_coverage agris
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
South Atlantic Ocean
genre_facet Antarc*
Antarctic
South Atlantic Ocean
op_source Remote Sensing; Volume 15; Issue 15; Pages: 3894
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs15153894
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15153894
container_title Remote Sensing
container_volume 15
container_issue 15
container_start_page 3894
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