从第三极到北极： 积雪变化研究进展
刘一静1(
), 孙燕华1, 钟歆玥2(), 王树发1, 肖雄新3, 马丽娟4, 苏航5, 赵文宇1, 张廷军1,6()
), 孙燕华1, 钟歆玥2(), 王树发1, 肖雄新3, 马丽娟4, 苏航5, 赵文宇1, 张廷军1,6()
Changes of snow cover in the Third Pole and the Arctic
Yijing LIU1(), Yanhua SUN1, Xinyue ZHONG2(), Shufa WANG1, Xiongxin XIAO3, Lijuan MA4, Hang SU5, Wenyu ZHAO1, Tingjun ZHANG1,6()
), Yanhua SUN1, Xinyue ZHONG2(), Shufa WANG1, Xiongxin XIAO3, Lijuan MA4, Hang SU5, Wenyu ZHAO1, Tingjun ZHANG1,6()
图8. 基于气象台站的欧亚大陆北部冬季最大积雪深度线性变化趋势（1966—2014年）［
图中仅显示平均变化趋势[cm·(10a)-1]在0.05水平上具有统计显著性的区域
Fig.8. Linear trend estimates （1966—2014） in the time series of maximum winter snow depth at meteorologicalstations［
The inset panel shows climate regions where the spatially-averaged trends [cm·(10a)-1] were statistically significant at the 0.05 level
