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Seasonal variations of eddy kinetic energy flux in the South Indian Countercurrent region

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Abstract

The inverse cascade flux of kinetic energy (KE) and its length scale in the South Indian Countercurrent (SICC) region were investigated using 24-year satellite altimeter daily data from 1993–2016. The evolution of the eddy life cycle in the SICC was presented systemically. It was found that the arrest and inject scales of inverse cascade were within the baroclinic most unstable scale and observed energy-containing eddy scale. The seasonal cycle of the arrest scale, inject scale, and amplitude of the inverse cascade were compared with the eddy kinetic energy seasonal cycle, which revealed a 1.5-month lag of the eddy kinetic energy to the vertical shear of zonal velocity, implying the existence of nonlinear processes during the eddy growth phase. Meanwhile, the anisotropy of the inverse cascade indicated that kinetic energy might be transferred from meridional motions to zonal motions, which is probably caused by β effect. These results would be beneficial for a better understanding of the KE transfer processes in the SICC region.

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Data Availability Statement

The altimeter products have been produced by DUACS with AVISO and distributed by CMEMS. Data could be downloaded from http://marine.copernicus.eu/. The product name is global ocean gridded L4 sea surface heights and derived variables reprocessed (1993-ongoing) and the identifier of product is SEALEVEL_GLO_PHY_L4_REP_OBSERVATION_008_047. The World Ocean Atlas 2018 (WOA18) dataset is available at https://www.nodc.noaa.gov/OC5/woa18/woa18data.html.

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Acknowledgment

We appreciate helpful discussion with Dr. LIU Chuanyu.

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Correspondence to Faming Wang.

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Supported by the National Natural Science Foundation of China (Nos. 41776035, 41676007) and the Funds for Creative Research Groups of China (No. 41421005)

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Chen, Z., Wang, F., Zheng, J. et al. Seasonal variations of eddy kinetic energy flux in the South Indian Countercurrent region. J. Ocean. Limnol. 38, 1464–1475 (2020). https://doi.org/10.1007/s00343-020-0115-5

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  • DOI: https://doi.org/10.1007/s00343-020-0115-5

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