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hydrological cycles on the surface. Lombardo for the urban climate is a system that covers the climate of a given land space and its urbanization is the result of human actions, combined with the geo-environmental aspects of the urban site. The vegetated areas present them selves as important agents softening temperature in the urban environment by promoting the reduction of energy consumption and increase air quality. Thus the aim of this article is to visualize the layout of the surface temperature for different targets present in the city of Recife by Landsat 5TM images and apply TsHARP to identify the influence of different building materials in the values of surface temperature. To this we used eight images of Landsat 5 TM orbital points and 214/65 and 66. All images were pre-processed and orthorectified. To obtain the surface temperature was used the methodology developed by Allen and Bastiaanssen an dresampling of the spatial resolution of the thermal band to 30m technique was used TsHARP proposed by Agam. It was observed that the vegetated areas were able to maintain lower temperatures in dry or rainy periods. In some cases vegetated areas had large difference with respect to eight degrees or constructed impermeable areas. Major projects and parking lots that had demonstrated good afforestation lower temperatures than who did not.

Use and Soil Cover and its Efects on Distribution of the Surface Temperature on Urban Area