For estimating evapotranspiration of landscape, in addition to vegetation coefficient, coefficients related to microclimate, plant density adjustment and specific plant species adjustment must also be calculated. In this study, using Landsat 7 satellite images and Mashhad Synoptic Station data, the actual evapotranspiration of landscape was calculated then, using climatic and environmental parameters obtained from satellite images and Seabl model, a relationship between microclimate coefficient and air temperature as well as relationship between density coefficient and normalized difference index of vegetation was established. Finally, the obtained relationships were evaluated by field monitoring of soil moisture in Ghadir Park of Mashhad. By determining the locations of field locations on the satellite image the relationship between NDVI index and the landscape density coefficient was investigated. The results showed that the best model presented using linear regression as Kd = 0.9941 * NDVI + 0.5058 with a correlation coefficient of 0.98 that the maximum percentage of error between calculated evapotranspiration for landscape using extracted relationships and measured values from moisture weight monitoring is less than 24%. due to severe water deficit in the forest landscape and insufficient water availability of the plant, evapotranspiration calculation using the Sabal model is inappropriate and has many errors. Therefore, instead of using the Sebal model, the extracted relationships can be used to determine the vegetation coefficients and the water requirement of urban landscape.