Reversal and amplification of zonal flows by boundary enforced thermal wind
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d="para0001">Numerical investigation of interaction of geostrophic and ageostrophic zonal flows.

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d="para0002">Reduction of equatorial heat flux leads to inverted geostrophic zonal flow system.

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d="para0003">Standard theoretical picture of zonal flow generation cannot explain these unexpected results.

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d="para0004">Confirmed by a broad numerical parameter study.

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