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根据１０个群体１２个气候及经纬度因子，并综合主分量和聚类两方面分析结果，我们认为红皮云杉可划为以下５个自然分布气候区：长白山气候区（Ｉ）；老爷岭、张广才岭、完达山气候区（Ⅱ）；小兴安岭气候区（Ⅲ）；大兴安岭北部气候区（Ⅳ）；大兴安岭西南部气候区（Ｖ）。从红皮云杉分布区来看，由西向东，蒸发量由大变小，降水量则由小变大，干到湿的气候生态模式。
Based on the 12 climatic and latitude and longitude factors of 10 groups and combining the principal components and cluster analysis results, we believe that the red spruce can be divided into the following five natural climatic zones: Changbai Mountain Climatic Zone (I); Laoyeling, Zhangguangcailing, Wandashan Climate Zone (Ⅱ); Xiaoxing’anling Climate Zone (Ⅲ); North Daxing’anling Climate Zone (Ⅳ); Southwestern Daxing’anling Climate Zone (V). From the distribution of spruce Picea, from west to east, the evaporation from larger to smaller, precipitation from small to large, dry to wet climate and ecological model.