Guo Xue-Mei, Wang Zhao-Peng, Zhang Nan, Zhang Dong-You
Heilongjiang Provincial Key Laboratory of Geographical Environment Monitoring and Spatial Information Service in Cold Region, Harbin Normal University, Harbin 150025, China.
School of Geography and Tourism, Xinjiang Normal University, Urumqi 830054, China.
Ying Yong Sheng Tai Xue Bao. 2021 Oct;32(10):3405-3414. doi: 10.13287/j.1001-9332.202110.042.
In the context of global warming, the increases of temperature may affect tree growth and thus disturb ecosystem balance. In this study, we explored the main limiting factors for radial growth of var. and in the Mohe area of Greater Khingan Mountains by using growth-climate response function analysis and moving correlation analysis, as well as the interspecific difference of the responses of radial growth to rapid warming. The results showed that the radial growth of var. and was affected by both temperature and precipitation. var. was more sensitive to climate change than , and its sensitivity to climate factors was more stable than The radial growth of var. was significantly positively correlated with the monthly mean temperature and the monthly mean minimum temperature of the growing season, while that of was significantly positively correlated with the monthly mean temperature and the monthly mean maximum temperature of winter. Precipitation in winter promoted the growth of var. , whereas precipitation in the late growing season of the previous year inhibited the radial growth of . After the rapid warming in 1990, the limiting effect of precipitation on var. changed from negative to significantly positive, with the inhibition effect of high temperature being greater than the promotion effect. The inhibitory effect of high temperature on was enhanced, and the limiting effect of precipitation on was also enhanced after heating up. The growth rate decreased significantly, with obvious difference being observed in the correlations between the growth rate of two species with temperature and precipitation. Our results could provide scientific basis for forest ecosystem management and protection in Greater Khingan Mountains.
在全球变暖的背景下,气温升高可能会影响树木生长,进而扰乱生态系统平衡。在本研究中,我们运用生长 - 气候响应函数分析和移动相关性分析,探究了大兴安岭漠河地区[具体树种1]变种和[具体树种2]径向生长的主要限制因素,以及径向生长对快速变暖响应的种间差异。结果表明,[具体树种1]变种和[具体树种2]的径向生长均受温度和降水的影响。[具体树种1]变种对气候变化比[具体树种2]更敏感,且其对气候因子的敏感性比[具体树种2]更稳定。[具体树种1]变种的径向生长与生长季月平均温度和月平均最低温度显著正相关,而[具体树种2]的径向生长与冬季月平均温度和月平均最高温度显著正相关。冬季降水促进了[具体树种1]变种的生长,而上一年生长季后期的降水则抑制了[具体树种2]的径向生长。1990年快速变暖后,降水对[具体树种1]变种的限制作用从负变为显著正,高温的抑制作用大于促进作用。高温对[具体树种2]的抑制作用增强,升温后降水对[具体树种2]的限制作用也增强。生长速率显著下降,两个树种的生长速率与温度和降水的相关性存在明显差异。我们的研究结果可为大兴安岭森林生态系统的管理和保护提供科学依据。