Correction to: Observation of submesoscale turbulence in a cyclonic eddy

Correction to: Ocean Dynamics

https://doi.org/10.1007/s10236-020-01349-5

The original version of this article unfortunately contained a mistake. During the production process, Fig. 4 was presented incorrectly which was the same as Fig. 5. The corrected figure is given here.

Fig. 4

Observed 6 zonal tracks average spectra and their decomposition at 48-m depth. a Observed kinetic energy and potential energy spectrum. The black, red, blue, and magenta lines are the spectra of kinetic energy K(k), longitudinal kinetic energy S^u(k), transverse kinetic energy S^v(k), and potential energy S^b(k). The dashed magenta line shows S^b(k) with wavenumbers larger than distinguishable resolution. The error bar represents 95% confidence limits. b The Helmholtz decomposition. The black, red, and blue lines are the spectra of observed kinetic energy K(k) into its rotational K^φ(k) and divergent K^ϕ(k) components. c Wave-vortex decomposition. The red and blue lines are the spectra of inertia-gravity wave component E^w(k) and the residual geostrophic component E^g(k). Observed geostrophic energy ${E}_{obs}^g(k)$ (magenta line) is calculated by temperature-salinity and residual inertia-gravity wave component ${E}_{obs}^w(k)$ (green line). The dashed lines show wavenumber greater than maximum distinguishable resolution

The original article has been corrected.