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大面积干扰遗留物与原始云杉林的气候敏感性。

Large-scale disturbance legacies and the climate sensitivity of primary Picea abies forests.

机构信息

Faculty of Forestry and Wood Sciences, Czech University of Life Sciences, Prague, Czech Republic.

School of Forest Resources, University of Maine, Orono, ME, USA.

出版信息

Glob Chang Biol. 2018 May;24(5):2169-2181. doi: 10.1111/gcb.14041. Epub 2018 Feb 16.

Abstract

Determining the drivers of shifting forest disturbance rates remains a pressing global change issue. Large-scale forest dynamics are commonly assumed to be climate driven, but appropriately scaled disturbance histories are rarely available to assess how disturbance legacies alter subsequent disturbance rates and the climate sensitivity of disturbance. We compiled multiple tree ring-based disturbance histories from primary Picea abies forest fragments distributed throughout five European landscapes spanning the Bohemian Forest and the Carpathian Mountains. The regional chronology includes 11,595 tree cores, with ring dates spanning the years 1750-2000, collected from 560 inventory plots in 37 stands distributed across a 1,000 km geographic gradient, amounting to the largest disturbance chronology yet constructed in Europe. Decadal disturbance rates varied significantly through time and declined after 1920, resulting in widespread increases in canopy tree age. Approximately 75% of current canopy area recruited prior to 1900. Long-term disturbance patterns were compared to an historical drought reconstruction, and further linked to spatial variation in stand structure and contemporary disturbance patterns derived from LANDSAT imagery. Historically, decadal Palmer drought severity index minima corresponded to higher rates of canopy removal. The severity of contemporary disturbances increased with each stand's estimated time since last major disturbance, increased with mean diameter, and declined with increasing within-stand structural variability. Reconstructed spatial patterns suggest that high small-scale structural variability has historically acted to reduce large-scale susceptibility and climate sensitivity of disturbance. Reduced disturbance rates since 1920, a potential legacy of high 19th century disturbance rates, have contributed to a recent region-wide increase in disturbance susceptibility. Increasingly common high-severity disturbances throughout primary Picea forests of Central Europe should be reinterpreted in light of both legacy effects (resulting in increased susceptibility) and climate change (resulting in increased exposure to extreme events).

摘要

确定森林干扰速率变化的驱动因素仍然是一个紧迫的全球变化问题。大规模的森林动态通常被认为是受气候驱动的,但很少有适当规模的干扰历史记录可供评估干扰遗留物如何改变随后的干扰速率以及干扰对气候的敏感性。我们从分布在整个欧洲的五个景观中的五个波希米亚森林和喀尔巴阡山脉的原始白云杉森林片段中编译了多个基于树木年轮的干扰历史记录。该区域年表包括 11595 个树木核心,其年轮日期涵盖 1750 年至 2000 年,从 37 个林分的 560 个清查样地中收集,分布在 1000 公里的地理梯度上,这是迄今为止在欧洲构建的最大干扰年表。十年一次的干扰速率随时间显著变化,在 1920 年后下降,导致树冠树龄普遍增加。目前约有 75%的树冠面积是在 1900 年前形成的。将长期干扰模式与历史干旱重建进行比较,并进一步与基于 LANDSAT 图像的林分结构和当代干扰模式的空间变化联系起来。历史上,每十年一次的帕尔默干旱严重程度指数最小值与树冠去除率较高相对应。当代干扰的严重程度随着每个林分自上次重大干扰以来的估计时间的增加而增加,随着平均直径的增加而增加,随着林分内结构变异性的增加而减少。重建的空间模式表明,历史上高的小尺度结构变异性降低了大规模干扰的易感性和对气候的敏感性。自 1920 年以来干扰率的降低,可能是 19 世纪高干扰率的遗留效应,导致该地区最近干扰易感性的增加。中欧原始白云杉林中日益常见的高严重度干扰应根据遗留效应(导致易感性增加)和气候变化(导致暴露于极端事件的增加)进行重新解释。

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