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Geographically Structured Growth decline of Rear-Edge Iberian Fagus sylvatica Forests After the 1980s Shift Toward a Warmer Climate

机译:20世纪80年代转向温暖的气候后,在20世纪80年代后,靠背伊比利亚的地理结构增长衰退

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Warming-related growth decrease on southern Fagus sylvatica forests has been observed in different regions; however, whether it is a generalized fact or not remains unclear. Here we investigate the geographical pattern on growth response of the southwestern European beech forests to the warming climate shift which started in the 1980s. We sampled 15 beech forests (215 trees) across four climatically contrasting regions (Mediterranean, Pyrenean, low- and high-elevation Atlantic areas) near the southern distribution limit of the species in the Iberian Peninsula. Dendrochronological analyses were carried out to evaluate the growth of European beech since the 1950s. Growth responses quantified as pointer years, abrupt growth changes and long-term growth trends were compared between periods (before and after the 1980s climate shift), geographical regions and tree sizes. Analyses of the studied variables indicated a growth decrease in basal area increment after the climate shift in three of the four studied regions. Pyrenean stands were not negatively influenced by the climate shift, although an increase in the frequency of negative abrupt growth changes was also found there. Growth after the climate shift presented divergent patterns depending on the geographical region. Although Mediterranean and Atlantic stands presented different indicators of constrained growth, Pyrenean stands showed rising long-term growth trends. Such results suggest that regional characteristics differentially determine the growth response of the southern European beech forests to recent warming periods. Iberian beech forests located at the Pyrenees would benefit from forecasted warming conditions, whereas Atlantic and Mediterranean forests would be more prone to suffer warming-related growth decline.
机译:在不同的地区观察到南部Fagus Sylvatica森林的温暖相关的增长减少;但是,是否是广义事实或不清楚不清楚。在这里,我们调查西南欧洲山毛榉森林增长反应的地理模式,以20世纪80年代开始的热情气候变化。在伊比利亚半岛南部分配限制的四个气候对比地区(地中海,Pyrenean,低高升和高海拔大西洋地区),我们将15个山毛榉森林(215棵树)进行了采样。自20世纪50年代以来,进行了分析分析以评估欧洲山毛榉的生长。在期间(在20世纪80年代气候变化之前和之后)之间比较了数量的成长响应,突然的增长变化和长期增长趋势,地理区域和树尺寸。研究的分析表明,在四个研究区域中的三个地区的气候变化后,基础区域增量的增长降低。 Pyrenean站立的气候变化不会产生负面影响,尽管在那里也发现了负突然生长变化的频率的增加。根据地理区域提出了气候变化呈现不同模式后的生长。虽然地中海和大西洋展台呈现出不同的约束增长指标,但Pyrenean立场表现出长期增长趋势上升。这些结果表明,区域特征差异地确定了南欧山毛榉森林的增长反应,以至于最近的变暖期。位于比利牛斯的伊比利亚山毛榉森林将受益于预测的温暖条件,而大西洋和地中海森林将更容易受到温暖相关的增长下降。

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