玉龙雪山不同海拔丽江云杉径向生长对气候变异的响应
张贇1,2,尹定财1,*(
),田昆1,2,张卫国1,和荣华3,和文清3,孙江梅3,刘振亚1,2
),田昆1,2,张卫国1,和荣华3,和文清3,孙江梅3,刘振亚1,2
Radial growth responses of Picea likiangensis to climate variabilities at different altitudes in Yulong Snow Mountain, southwest China
ZHANG Yun1,2,YIN Ding-Cai1,*(),TIAN Kun1,2,ZHANG Wei-Guo1,HE Rong-Hua3,HE Wen-Qing3,SUN Jiang-Mei3,LIU Zhen-Ya1,2
),TIAN Kun1,2,ZHANG Wei-Guo1,HE Rong-Hua3,HE Wen-Qing3,SUN Jiang-Mei3,LIU Zhen-Ya1,2
图4. 丽江云杉残差年表与主要气候因子的滑动响应分析。虚线为95%置信区间。L, 低海拔; M, 中海拔; H, 高海拔。
Fig. 4. Moving interval response analysis between the residual chronologies and main climatic factors. Dotted lines indicate the 95% confidence level. L, low altitude; M, intermediate altitude; H, high altitude.
