Temperature and precipitation are the primary factors that impact the distribution of snow, with terrain exerting an indirect influence on both (Namias. 1985,Tong et al. 2009). In areas with high wind conditions, particularly on plateau surfaces and mountain peaks, wind-blown snow is highly likely to accumulate, resulting in the redistribution of snow. Additionally, radiation plays a significant role in the melting process of snow (Fujita et al. 2010,Golding et al. 1986). Additionally, the type of subsurface has a significant impact on surface albedo, radiation reception, and surface roughness, among other factors. It also has an intercepting effect on the snowpack (Jost et al. 2007). In this study, a comprehensive selection of 33 environmental factors was made to analyze the dominant factors influencing the distribution pattern of the stable snowpack in the selected study area (see Table 1). The selection of these factors took into full consideration both the snowpack influencing factors and the unique natural conditions of the study area.