Decadal Variability of Eddy Kinetic Energy Along the Eastern Boundary of the Subtropical South Indian Ocean

Abstract Using more than three decades (1993–2024) of satellite altimetry and ocean reanalysis, we reassess the dominant timescales of low‐frequency mesoscale eddy variability along the eastern boundary of the subtropical South Indian Ocean. After removal of the seasonal cycle, eddy kinetic energy (EKE) is primarily modulated on decadal timescales (8–16 years), with a pronounced spectral peak near 10–12 years, whereas interannual variability (2–7 years) is comparatively weak. Decadal EKE variability is governed by baroclinic instability associated with vertical shear between the poleward Leeuwin Current (LC) and the equatorward Leeuwin Undercurrent. Decadal changes in LC strength dominate shear variability and are strongly linked to Pacific decadal forcing. These findings improve our understanding of the dynamics of mesoscale eddies in this dynamically distinct eastern boundary system.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-04-25
DOI
https://doi.org/10.1029/2025gl120546
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
0.00

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article

Decadal Variability of Eddy Kinetic Energy Along the Eastern Boundary of the Subtropical South Indian Ocean

Xuhua Cheng, Yifei Zhou
Geophysical Research Letters
Oceanographic and Atmospheric Processes
article

Decadal Variability of Eddy Kinetic Energy Along the Eastern Boundary of the Subtropical South Indian Ocean

Xuhua Cheng, Yifei Zhou
article en

Abstract

Abstract Using more than three decades (1993–2024) of satellite altimetry and ocean reanalysis, we reassess the dominant timescales of low‐frequency mesoscale eddy variability along the eastern boundary of the subtropical South Indian Ocean. After removal of the seasonal cycle, eddy kinetic energy (EKE) is primarily modulated on decadal timescales (8–16 years), with a pronounced spectral peak near 10–12 years, whereas interannual variability (2–7 years) is comparatively weak. Decadal EKE variability is governed by baroclinic instability associated with vertical shear between the poleward Leeuwin Current (LC) and the equatorward Leeuwin Undercurrent. Decadal changes in LC strength dominate shear variability and are strongly linked to Pacific decadal forcing. These findings improve our understanding of the dynamics of mesoscale eddies in this dynamically distinct eastern boundary system.

Geophysical Research LettersVol. 53(8)
Hohai University (CN), Ministry of Natural Resources (CN)
National Natural Science Foundation of China, Fundamental Research Funds for the Central Universities
Life below water
Openalex Percentile: Top 10%
Oceanographic and Atmospheric Processes
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