A. Over an ocean surface, the Bowen ratio is estimated to be about 0.2. Estimate the sensible and latent heat fluxes to the atmosphere, as well as the rate of evaporation, from the ocean surface, when the net radiation received just above the surface is 600 W m the heat flux to the water below 50 m is negligible, the rate of warming of the 50 m deep oceanic mixed layer is 0.08°C day-, and the sea surface temperature is 25°C. B. What will be the rate of warming or cooling of the 50 m deep oceanic mixed layer at the time of intense cold-air advection when the Bowen ratio is estimated to be 0.5, the net radiation los from the surface is 50 W m and the rate of evaporation is 2.3 kg ms?