. The effect of stochastic surface heat fluxes on the climatology of the seasonal thermocline. . TIME (DAYS) HBRR - HZERO u U o 0- o U ri °8 NO. DF YERRS 100) i i i ^ 1 r T i i i TIME (DAYS) Figure depth statistics-full model. a) The variance in the mixed layer depth over the The difference between the average when randomly forced and the mixed is the product of the annual cycle experiment. m b) mixed layer depch layer depth which alo

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. The effect of stochastic surface heat fluxes on the climatology of the seasonal thermocline. . TIME (DAYS) HBRR - HZERO u U o 0- o U ri °8 NO. DF YERRS 100) i i i ^ 1 r T i i i TIME (DAYS) Figure depth statistics-full model. a) The variance in the mixed layer depth over the The difference between the average when randomly forced and the mixed is the product of the annual cycle experiment. m b) mixed layer depch layer depth which alone, h-ho. 36

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Keywords: ., bookcentury1900, booksubjectmeteorology, booksubjectoceanography