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由于持续的水分限制,预计欧洲山毛榉在北部边缘不会有未来的生长增强。

No Future Growth Enhancement Expected at the Northern Edge for European Beech due to Continued Water Limitation.

机构信息

Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, Switzerland.

Oeschger Centre for Climate Change Research, Bern, Switzerland.

出版信息

Glob Chang Biol. 2024 Oct;30(10):e17546. doi: 10.1111/gcb.17546.

Abstract

With ongoing global warming, increasing water deficits promote physiological stress on forest ecosystems with negative impacts on tree growth, vitality, and survival. How individual tree species will react to increased drought stress is therefore a key research question to address for carbon accounting and the development of climate change mitigation strategies. Recent tree-ring studies have shown that trees at higher latitudes will benefit from warmer temperatures, yet this is likely highly species-dependent and less well-known for more temperate tree species. Using a unique pan-European tree-ring network of 26,430 European beech (Fagus sylvatica L.) trees from 2118 sites, we applied a linear mixed-effects modeling framework to (i) explain variation in climate-dependent growth and (ii) project growth for the near future (2021-2050) across the entire distribution of beech. We modeled the spatial pattern of radial growth responses to annually varying climate as a function of mean climate conditions (mean annual temperature, mean annual climatic water balance, and continentality). Over the calibration period (1952-2011), the model yielded high regional explanatory power (R = 0.38-0.72). Considering a moderate climate change scenario (CMIP6 SSP2-4.5), beech growth is projected to decrease in the future across most of its distribution range. In particular, projected growth decreases by 12%-18% (interquartile range) in northwestern Central Europe and by 11%-21% in the Mediterranean region. In contrast, climate-driven growth increases are limited to around 13% of the current occurrence, where the historical mean annual temperature was below ~6°C. More specifically, the model predicts a 3%-24% growth increase in the high-elevation clusters of the Alps and Carpathian Arc. Notably, we find little potential for future growth increases (-10 to +2%) at the poleward leading edge in southern Scandinavia. Because in this region beech growth is found to be primarily water-limited, a northward shift in its distributional range will be constrained by water availability.

摘要

随着全球持续变暖,日益严重的水资源短缺对森林生态系统造成生理压力,对树木的生长、活力和存活产生负面影响。因此,了解单个树种将如何应对日益增加的干旱压力是解决碳核算和制定气候变化缓解策略的关键研究问题。最近的树木年轮研究表明,高纬度地区的树木将受益于温暖的气温,但这在很大程度上依赖于物种,对于更温和的树种则知之甚少。利用一个独特的泛欧欧洲山毛榉(Fagus sylvatica L.)树轮网络,该网络由 2118 个地点的 26430 棵欧洲山毛榉组成,我们应用了一个线性混合效应模型框架来:(i) 解释气候依赖性生长的变化;(ii) 预测整个山毛榉分布范围内的近期(2021-2050 年)的生长情况。我们将径向生长对逐年变化的气候的空间模式建模为平均气候条件(年平均温度、年平均气候水平衡和大陆性)的函数。在校准期(1952-2011 年)内,该模型在区域解释能力方面表现出色(R=0.38-0.72)。考虑到一个中等程度的气候变化情景(CMIP6 SSP2-4.5),未来山毛榉的生长预计将在其大部分分布范围内减少。特别是,在西北中欧和地中海地区,预计生长减少 12%-18%(四分位距)。相比之下,气候驱动的生长增加仅限于当前出现的约 13%的地区,这些地区的历史年平均温度低于~6°C。更具体地说,模型预测阿尔卑斯山脉和喀尔巴阡弧形山脉的高海拔集群的生长增加 3%-24%。值得注意的是,我们发现,在斯堪的纳维亚南部的极地处,未来的生长增加潜力很小(-10%至+2%)。因为在这个地区,山毛榉的生长主要受到水分限制,所以其分布范围的北移将受到水分供应的限制。

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