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. 2018 Aug 7;115(34):8499–8504. doi: 10.1073/pnas.1805927115

Fig. 2.

Fig. 2.

(A and B) The kinetic energy Q(r) of the equatorially antisymmetric zonal flow derived from the shallow cloud-level winds model as a function of r/R (A) and the profile of Q(r) derived from the deep cloud-level winds model as a function of r/R (B).