MODIFICATION OF THE SNOW COVER THICKNESS IN THE TRANSCARPATHIAN REGION BETWEEN 1961 AND 2010
DOI:
https://doi.org/10.32782/2786-5843/2026-3-4Keywords:
climate change, snow cover thickness, Transcarpathia, linear trends, cartographic methods, krigingAbstract
Relevance of the research: Global climate change has come to the forefront among environmental problems; along with global and regional climate warming, increasing attention is being paid to related climatic elements such as changes in snow cover. The subject of the research is changes in snow cover thickness in Transcarpathia during the period 1961–2010. The aim of the research is to identify the features of changes in the thickness of snow cover in Transcarpathia over recent decades, and to reveal possible causes of modifications. Research methods: to identify changes, statistical analysis methods were used, primarily trend analysis, and their geographical features were studied using cartographic visualization and analysis methods. The results of the study: The analysis revealed significant geographical differences in the average snow cover thickness in Transcarpathia in 1961–2010: it ranged from 7 to 124 cm, depending mainly on elevation above sea level and slope aspect. During the study period, snow cover thickness decreased across most of Transcarpathia, except for the highest mountain ridges. Although statistically significant changes at the 95% confidence level were detected only in limited areas, the rate of decrease in the Transcarpathian Lowland and the Pre-Carpathian region reached 10–15% per decade. Practical significance: the results contribute to a better understanding the regional consequences of climate change, including changes in snow cover, and contribute to the adaptation of human activities, in particular ski tourism, to them. Conclusions: the thickness of the snow cover in Transcarpathia is changing due to warming, but the features of the changes have significant spatial differences. The prospect of further research: the results can be used as a basis for further analysis, in particular to identify breakpoints in the time series of snow cover data.
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