New-modelled climate change scenarios were modified especially for Slovak conditions and used for identification of climate change impact on soil resources of Slovak Republic. Based on it, a "pedoclimatic scenario” was formulated and produced reflecting changes of soil cover of Slovakia with following elaboration of the predicted pedogenetic processes including degraded ones. Our temperate climatic zone will probably cause only small changes in soil genesis compared with other climatic zones. Slow retrograding development of soils and catenas will be dominate along with time horizons defined by climatologists; the majority of genetic soil units at type and subtype level will not change. Changes will be first recognizable in the surface soil layer as this is the most susceptible part to moisture and temperature. A marked acceleration of erosion processes, locally also gleyic and salinization processes are expected, It will be necessary to monitor and control them. More expressive and significant changes will strike some particular soil properties and characteristics. Loss of organic carbon will have the decisive impact on soil structure and soil fertility. The plant nutrient dynamics predetermined by the climatic change will be negligible. Some mitigation and stabilization measurement proposals are described with respect to farmland of Slovakia.