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Aurélie J. Moulin, James N. Moum, and Emily L. Shroyer

as steady state. Finally, there is a brief period of decay at the end of the heating cycle. In sum, we have shown a consistent pattern of mixing in the diurnal warm layer, in this case associated with the strong insolation of the tropics. While the signal may be more subtle away from the tropics, the general pattern ought to hold elsewhere, save for a poleward-increasing Coriolis veering of the diurnal jet. The phasing between air–sea fluxes and the ocean’s response, which in part is determined

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