Extended Data Fig. 7: Decomposition of \(Q_{{\mathrm{eddy}},{\mathrm{v}}}^{\upomega ,{\mathrm{sub}}}\) into different dynamical components. | Nature Geoscience

Extended Data Fig. 7: Decomposition of \(Q_{{\mathrm{eddy}},{\mathrm{v}}}^{\upomega ,{\mathrm{sub}}}\) into different dynamical components.

From: El Niño/Southern Oscillation inhibited by submesoscale ocean eddies

Extended Data Fig. 7: Decomposition of $$Q_{{\mathrm{eddy}},{\mathrm{v}}}^{\upomega ,{\mathrm{sub}}}$$ Q eddy , v ω , sub into different dynamical components.The alternative text for this image may have been generated using AI.

a, Vertical profiles of time-mean \(Q_{{\mathrm{eddy}},{\mathrm{v}}}^{\upomega ,{\mathrm{sub}}}\) averaged over the Niño3.4 region during 1920–1929 and its decomposition into different components. b, Time series of \(Q_{{\mathrm{eddy}},{\mathrm{v}}}^{\upomega ,{\mathrm{sub}}}\) at 50 m and its decomposition into different components at 50 m averaged over the Niño3.4 region. See ‘Decomposing vertical submesoscale eddy heat flux into different ocean dynamics’ in Methods for the meanings of labels.

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