Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, Virginia, USA.
Forest Global Earth Observatory, Smithsonian Tropical Research Institute, Panama, Republic of Panama.
Glob Chang Biol. 2022 Jan;28(1):245-266. doi: 10.1111/gcb.15934. Epub 2021 Oct 30.
Tree rings provide an invaluable long-term record for understanding how climate and other drivers shape tree growth and forest productivity. However, conventional tree-ring analysis methods were not designed to simultaneously test effects of climate, tree size, and other drivers on individual growth. This has limited the potential to test ecologically relevant hypotheses on tree growth sensitivity to environmental drivers and their interactions with tree size. Here, we develop and apply a new method to simultaneously model nonlinear effects of primary climate drivers, reconstructed tree diameter at breast height (DBH), and calendar year in generalized least squares models that account for the temporal autocorrelation inherent to each individual tree's growth. We analyze data from 3811 trees representing 40 species at 10 globally distributed sites, showing that precipitation, temperature, DBH, and calendar year have additively, and often interactively, influenced annual growth over the past 120 years. Growth responses were predominantly positive to precipitation (usually over ≥3-month seasonal windows) and negative to temperature (usually maximum temperature, over ≤3-month seasonal windows), with concave-down responses in 63% of relationships. Climate sensitivity commonly varied with DBH (45% of cases tested), with larger trees usually more sensitive. Trends in ring width at small DBH were linked to the light environment under which trees established, but basal area or biomass increments consistently reached maxima at intermediate DBH. Accounting for climate and DBH, growth rate declined over time for 92% of species in secondary or disturbed stands, whereas growth trends were mixed in older forests. These trends were largely attributable to stand dynamics as cohorts and stands age, which remain challenging to disentangle from global change drivers. By providing a parsimonious approach for characterizing multiple interacting drivers of tree growth, our method reveals a more complete picture of the factors influencing growth than has previously been possible.
树木年轮为了解气候和其他驱动因素如何塑造树木生长和森林生产力提供了宝贵的长期记录。然而,传统的树木年轮分析方法并非旨在同时测试气候、树木大小和其他驱动因素对个体生长的影响。这限制了检验有关树木对环境驱动因素的生长敏感性及其与树木大小相互作用的生态相关假说的潜力。在这里,我们开发并应用了一种新方法,即在广义最小二乘模型中同时模拟主要气候驱动因素、重建胸径(DBH)和日历年份的非线性效应,这些模型考虑了每个个体树木生长中固有的时间自相关性。我们分析了来自全球 10 个分布地点的 40 个物种的 3811 棵树木的数据,结果表明,降水、温度、DBH 和日历年份在过去 120 年中对树木的年生长都具有累加性,并且通常具有交互作用。生长响应主要对降水呈正相关(通常在≥3 个月的季节窗口内),对温度呈负相关(通常在≤3 个月的季节窗口内为最高温度),其中 63%的关系呈凹形下降。气候敏感性通常随 DBH 而变化(45%的情况进行了测试),较大的树木通常更敏感。小 DBH 时的年轮宽度趋势与树木建立时的光照环境有关,但基面积或生物量增量始终在中等 DBH 处达到最大值。考虑到气候和 DBH,92%的次生林或干扰林的物种的生长速度随时间下降,而在较老的森林中,生长趋势则较为复杂。这些趋势在很大程度上归因于林分动态,因为林分随年龄增长,这仍然难以从全球变化驱动因素中分离出来。通过提供一种简洁的方法来描述树木生长的多个相互作用的驱动因素,我们的方法比以前更全面地揭示了影响生长的因素。