CAJ | 학술논문

采用2009年和2010年2月中旬雪深、分层积雪密度、含水率和温度野外调查数据，分析了北疆地区积雪参数属性特征，雪深-温度和密度-含水率的关系。①雪深达10cm，雪土界面温度比积雪表面高3℃左右，超过10cm，偏高6～10℃；雪土界面温度与积雪深度呈高度线性相关，积雪越深，保温作用越显著；②2010年1月以来，北疆地区多降雪天气，2月积雪深度比2009年同期雪深明显增加；③2010年2月，北疆地区积雪密度均值总体范围在0．15～0．272g／cm^3，比2009年同期积雪密度0．087～0．225g/cm^3偏大；④在一定体积含水率间隔范围，积雪密度和体积含水率问呈线性相关。
채용2009년화2010년2월중순설심、분층적설밀도、함수솔화온도야외조사수거，분석료북강지구적설삼수속성특정，설심-온도화밀도-함수솔적관계。①설심체10cm，설토계면온도비적설표면고3℃좌우，초과10cm，편고6～10℃；설토계면온도여적설심도정고도선성상관，적설월심，보온작용월현저；②2010년1월이래，북강지구다강설천기，2월적설심도비2009년동기설심명현증가；③2010년2월，북강지구적설밀도균치총체범위재0．15～0．272g／cm^3，비2009년동기적설밀도0．087～0．225g/cm^3편대；④재일정체적함수솔간격범위，적설밀도화체적함수솔문정선성상관。
By using snow depth, snow-layers density, water content and snow-layer temperature data of northern Xinjiang in mid-February of 2009 and 2010,this study analyzed the property features of snow parameters and their relationships. The results showed that, ①The temperature of snow-soil interface was about 3 ℃ higher than the snow surface when snow depth was 10 cm,so did 6-10 ℃ with snow depth more than 10 cm. There was a linear correlation between snow-soil interface temperature and snow depth; the deeper the snow cover,the more significant the holding thermal effect. ②With more snow weather in northern Xinjiang since January 2010,snow depth in February 2010 was significantly higher than that in 2009 over the same period. ③Mean snow density range of 0.15-0.272 g/cm^3 in February 2010 was higher than that in 2009 with snow density range of 0.087-0.225 g/cm^3 through Northern Xinjiang. ④In certain interval range of volumetric water content, the snow density linearly correlated with the volume water content.