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Fine-Scale Eddies Detected by SWOT in the Kuroshio Extension
by
Du, Tianshi
, Jing, Zhao
in
altimeter
/ Altimeters
/ Altimetry
/ Amplitudes
/ Data processing
/ Datasets
/ Eddies
/ fine-scale eddies
/ Identification
/ Kuroshio Extension
/ Mechanical properties
/ Mesoscale phenomena
/ Methods
/ Observations
/ Ocean circulation
/ Ocean currents
/ Satellites
/ Sea level
/ Surface water
/ SWOT
/ Topographical drawing
/ topography
/ Vortices
2024
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Fine-Scale Eddies Detected by SWOT in the Kuroshio Extension
by
Du, Tianshi
, Jing, Zhao
in
altimeter
/ Altimeters
/ Altimetry
/ Amplitudes
/ Data processing
/ Datasets
/ Eddies
/ fine-scale eddies
/ Identification
/ Kuroshio Extension
/ Mechanical properties
/ Mesoscale phenomena
/ Methods
/ Observations
/ Ocean circulation
/ Ocean currents
/ Satellites
/ Sea level
/ Surface water
/ SWOT
/ Topographical drawing
/ topography
/ Vortices
2024
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Do you wish to request the book?
Fine-Scale Eddies Detected by SWOT in the Kuroshio Extension
by
Du, Tianshi
, Jing, Zhao
in
altimeter
/ Altimeters
/ Altimetry
/ Amplitudes
/ Data processing
/ Datasets
/ Eddies
/ fine-scale eddies
/ Identification
/ Kuroshio Extension
/ Mechanical properties
/ Mesoscale phenomena
/ Methods
/ Observations
/ Ocean circulation
/ Ocean currents
/ Satellites
/ Sea level
/ Surface water
/ SWOT
/ Topographical drawing
/ topography
/ Vortices
2024
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Fine-Scale Eddies Detected by SWOT in the Kuroshio Extension
Journal Article
Fine-Scale Eddies Detected by SWOT in the Kuroshio Extension
2024
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Overview
Conventional altimetry has greatly advanced our understanding of mesoscale eddies but falls short in studying fine-scale eddies (<150 km). The newly launched Surface Water and Ocean Topography (SWOT) altimeter, however, with its unprecedented high-resolution capabilities, offers new opportunities to observe these fine-scale eddies. In this study, we use SWOT data to explore these previously elusive fine-scale eddies in the Kuroshio Extension. During SWOT’s fast sampling phase from 29 May 2023 to 10 July 2023, we identified an average of 4.5 fine-scale eddies within each 120 km wide swath. Cyclonic eddies, which are slightly more frequent than the anticyclonic ones (ratio of 1.16), have a similar mean radius of 23.4 km. However, cyclonic eddies exhibit higher amplitudes, averaging 3.5 cm compared to 2.8 cm for anticyclonic eddies. In contrast to the mesoscale eddies detected by conventional altimeters, the fine-scale eddies revealed by SWOT are characterized by smaller sizes and weaker amplitudes. This study offers a preliminary view of fine-scale eddy characteristics from space, highlighting SWOT’s potential to advance our understanding of these dynamic processes. Nonetheless, it also emphasizes the necessity for comprehensive analysis to fully exploit the satellite’s capabilities in monitoring and interpreting complex eddy behaviors.
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