南盘江流域云南松径向生长对气候暖干化的响应
申佳艳1,李帅锋1,黄小波1,雷志全2,施兴全2,苏建荣1,*(
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Radial growth responses to climate warming and drying in Pinus yunnanensis in Nanpan River Basin
SHEN Jia-Yan1,LI Shuai-Feng1,HUANG Xiao-Bo1,LEI Zhi-Quan2,SHI Xing-Quan2,SU Jian-Rong1,*()
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图8. 云南松年轮宽度年表与上年5月至当年11月主要气候因子的滑动响应分析, 滑动窗口为25年, 偏移1年。A, 云南松径向生长与月平均气温(Tmp)的滑动响应分析。B, 云南松径向生长与月降水量(Pre)的滑动响应分析。C, 云南松径向生长与帕尔默干旱指数(PDSI)的滑动响应分析。
Fig. 8. Sliding response analysis of ring width chronology in Pinus yunanensis with main climatic factors from May of the previous year to November of the current year. The window size is 25 years, and the windows have been offset by one year. A, Sliding response analysis of radial growth and monthly mean temperature (Tmp). B, Sliding response analysis of radial growth and monthly precipitation (Pre). C, Sliding response analysis of radial growth and Palmer Drought Standard Index (PDSI).
