Method of Assessing the Influence of Snow and Vegetation Cover on the Thermal Regime of Soils Using the Example of the Msu Weather Station

This chapter delves into the methodology of assessing the influence of snow and vegetation cover on the thermal regime of soils, using the MSU weather station as a case study. It explores the role of seasonal freezing and thawing layers in thermal processes, emphasizing the importance of annual heat turnover and heat transfer. The study involves drilling boreholes and placing temperature sensors to compare the thermal regimes of soils with and without vegetation and snow cover. Key findings include the construction of thermal isopleths, which illustrate temperature variations over time and depth. The results highlight the significant impact of snow and vegetation cover on soil temperature, providing insights into the warming effect of cover in engineering and thermophysical calculations. This research is crucial for understanding the thermal dynamics of permafrost soils and their implications in the context of climate change.