The exchange of vertical energy occurs through the evaporation of the water and posterior condensation of the vapor, liberating latent heat, for the conduction of sensible heat of the terrestrial surface for atmosphere and through the convection that is the turbulent diffusion of heat of the terrestrial surface in direction the atmosphere. Such mechanisms of heat exchange occur of vertical form, that is, of the surface in direction the atmosphere, and are important for the maintenance of the thermal balance in the interface terrestrial atmosphere-surface. The horizontal exchange of heat occurs mainly through the transference of sensible heat in direction to the polar regions, for primary the atmospheric circulation and oceanic chains of the low latitudes. Another form of transference of horizontal heat is through the heat release latent that vapor d occurs when? water originated in the areas of low latitude if dirigem in direction to the polar regions, and if they condense in the atmosphere. Contact information is here: Anchin. (AYOADE, 1986) Beyond the circuit atmosphere-surface also the rocking of energy for the terrestrial surface exists that is one ' ' used concept in the Climatologia to relate the flow of liquid radiation to the transference of latent heat and heat sensvel' ' (AYOADE, 1986, P. 39). In the terrestrial surface the energy rocking can vary the latitude in accordance with, with the distribution of the surfaces eliminates and terrestrial, of the period of the year, and the flows of transference of the latent and sensible heat in the continental and terrestrial regions of the globe. In the generality, as much in continental areas as in oceanic the biggest values of liquid radiation is found in the tropics mainly for the effect of the solar radiation in the regions of low latitude, where the position of the Land in relation to the Sun, forms straight angles in tangent with the terrestrial surface, what potencializa the absorption and diminishes Albedo.