Zhao Ying, Cai Li-Xin, Jin Yu-Ting, Li Jun-Xia, Cui Di, Chen Zhen-Ju
Tree-Ring Laboratory, College of Forestry, Shenyang Agricultural University, Shenyang 110866, China.
Qingyuan Forest CERN, Chinese Academy of Sciences, Shenyang 110164, China.
Ying Yong Sheng Tai Xue Bao. 2021 Oct;32(10):3459-3467. doi: 10.13287/j.1001-9332.202110.034.
Plantation ecosystems are more vulnerable than natural ones to global climate change. Using the dendrochronology method, we established tree-ring width chronologies of distributed in the semi-arid region of Northeast China. We examined its growth dynamics, analyzed the relationship between radical growth and climate factors, and explored the effects of global warming on the growth and distribution of . The results showed that tree-ring width chronologies of were negatively correlated with mean temperature of growing season (May-July), and positively correlated with precipitation and Palmer drought severity index (PDSI) in the early growing season (April) and in the growing season (May-July). Water availability was the main limiting factor for the radial growth of . Along the increasing precipitation gradient from southwest to northeast, tree growth became more sensitive to annual mean temperature, and the correlation with annual precipitation shifted from positive to negative, indicating that tree growth in the relative arid area (southwest of the study area) was more severely restricted by water availability. Drought stress caused by climate warming resulted in growth declines at some sites in the southwest area. With the continuous warming-drying climate, the distribution boundary of in the study area would shrink locally, with the suitable growth boundary moving northward.
人工林生态系统比自然生态系统更容易受到全球气候变化的影响。利用树木年代学方法,我们建立了分布于中国东北半干旱地区的树木年轮宽度年表。我们研究了其生长动态,分析了径向生长与气候因子之间的关系,并探讨了全球变暖对其生长和分布的影响。结果表明,该树木年轮宽度年表与生长季(5 - 7月)平均温度呈负相关,与生长季前期(4月)及生长季(5 - 7月)的降水量和帕尔默干旱严重度指数(PDSI)呈正相关。水分有效性是该树种径向生长的主要限制因素。沿着从西南向东北降水量增加的梯度,树木生长对年平均温度变得更加敏感,与年降水量的相关性从正相关转变为负相关,这表明相对干旱地区(研究区域西南部)的树木生长受到水分有效性的限制更为严重。气候变暖导致的干旱胁迫致使西南部部分地区的树木生长下降。随着气候持续变暖和变干,研究区域内该树种的分布边界将局部收缩,适宜生长边界向北移动。