рельєф

The results of the comparison of archival topographic maps with materials tacheometry are presented. Found that the existing maps are outdated and do not provide objective information about the relief area. The possibilities of the program with respect to WEPP modeling of water erosion are shown.

The possibility of geoinformation terrain analysis using for the purpose of spatial estimation of soil moisture is shown. The analysis of the individual parameters of the relief affecting the spatial heterogeneity of topsoil moisture. It is proved that the coefficient of xeromorphic most suitable for the prediction of automorphic soil moisture.