A numerical investigation on the interaction of turbulent and long-wave radiative fluxes in the surface layer

摘要: The interaction of turbulent and radiative transfer applied to a number plausible atmospheric situations in the surface layer under stably stratified condition is discussed. calculated results show that long-wave flux has great influence upon thermal structure layer, it usually acts such way as weaken thickness constant heat layer. In case low wind velocities strongly stable stratifications, will become very thin and/or inexistent.