The Environment

The distribution of the surfaces eliminates and terrestrial they influence directly in the distribution of solar radiation on the surface, over all, for the continentalidade effect and of maritimidade, that is, the continental surfaces, data its thermodynamic and physical characteristics are cooled and suddenly heated with lesser necessity of profit caloric, in contrast, the maritime surfaces need the least three times more energy for can reach the same thermal saturation of a continental surface with the same dimensions, moreover, the water is cooled and heated of slower form, causing gradual differences in the thermal behavior of the Land in function of the distribution of the surfaces you eliminate and terrestrial. (AYOADE, 1986) the rise and the behavior of surfaces also affect the dynamics of distribution of the solar radiation, over all in local environments in microscale, therefore next to the level to the sea the amount of insolation received for the surface lesser must the occured attenuation for the great mass of the overlapping atmosphere to the environment to the level of the sea, already in high altitudes the volume of air mass on a point of the surface is minor what it causes to the reduction of the attenuation of the solar ray due the reduction of the volume that the same will have that to exceed until arriving the surface. Thus, the factors that influence in the amount of incident radiation in the Land can act in distinct scales, as well as they interact between itself in the dynamics of the solar radiation and in global the thermal behavior. The balance enters the amount of all energy that is absorbed and reflected for the Land it will form an annual report of energy that enters and leaves the terrestrial system, therefore, according to Ayoade ' ' radiation rocking means the difference between amount of radiation that is absorbed and emitted for data body or superfcie' '.