Latitudinal gradient in the meridional eddy momentum flux, the vertical gradient in the vertical eddy momentum flux, and their sum (as a function of latitude, φ and height, z), are shown as the top, middle and bottom rows, respectively (see text and Appendix C for details), after 1000 days. The left and right columns then show data for the Std Full and Std RT simulation, respectively (see Table 2 for explanation of simulation names).
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