Observations also depict a reduction in outgoing longwave radiation during the preonset phase Johnson et al. The evolution of Q 1 largely reflects the diurnal cycle of radiative heating, though enhanced warming near and within the boundary layer relates to the large convergence of eddy heat flux due to surface warming as the mixed layer deepens Johnson et al. View larger version 23K Fig. Studies demonstrate that this diurnal cycle is key to rectifying the slower i. Journal of the Atmospheric Sciences October , Vol. Soares, : Sensitivity of moist convection to environmental humidity.
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