Spruce is one of the economically most important woods forest tree species in Centraland Northern Europe economically. However, global climate change warming issignificantly changing the growth conditions and spruce is suffering from drought inmany places. The thesis focuses on quantifying the impact of climate change on theradial spruce growth of spruce in the Spiš region, which has been attacked by sulfur,nitrogen and heavy metal emissions in the past. In this work, we evaluated analysed a dendrochronological material collected in the a research area of Smolnícka sawmillpíla.We compared dendrochronological records with climatic data sourced from the nearestweather station Štós -– Kúpele,. The weather station is located at an altitude of 590 mabove sea level.Our results showed that only younger trees with lower thickness and age are morecorrelated with climate dataat lower elevations expressed statistically clear correlationswith some climate variables. The thesis also points out that the variability of radialincrements between trees greatly influences the interpretation of results. We found thatfor our chosen categories, in which we created average chronologies, they were notrepresented by a sufficient number of samples. We also found out that the results is aresignificantly influenced by the choice of the appropriate mathematical function for tostandardisezation tree-ring width series. Although several some of the results weresignificant statistically clear and logical, the insufficient number of samples in theselected categories affected the interpretation potential of the results. It would thereforebe necessary to either increase the number of samples in the territory or use othermethods for statistical evaluation in the future.