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首页> 外文期刊>Dendrochronologia >Growth-climate responses indicate shifts in the competitive ability of European beech and Norway spruce under recent climate warming in East-Central Europe
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Growth-climate responses indicate shifts in the competitive ability of European beech and Norway spruce under recent climate warming in East-Central Europe

机译:生长气候响应表明欧洲山毛榉和挪威云杉竞争能力的转变在最近在东部 - 中欧气候变暖下

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摘要

Long-term changes in climate substantially affect the tree growth and species distribution in Europe. In the presented study, the radial growth of Fagus sylvatica (L.) and Picea abies ((L.) Karst.) has been studied along an altitudinal gradient covering six vegetation formations characteristic for sub-montane, montane and high-montane conditions of the western Carpathians. Tree growth responses to temperature and precipitation changes have been analysed based on the sample of increment cores and standard dendroclimatic methods in two time periods, the reference period 1961-1990 and the recent period 1991-2012. The growth responses of spruce and beech to recent changes in climate were similar up to high-montane zones, where the beech shows significantly larger improvements of radial increments in comparison to spruce. The growth responses were mainly temperature driven. In the sub-montane area, the increased effect of precipitation in the recent period was overridden by the negative effects of warming, and the alleviated temperature limitation had an evidently supportive effect on tree growth in montane and high-montane areas. In the near future, the warming will likely cause decline in radial increments of beech and spruce in sub-montane areas due to expected landscape drying. At the same time, the improved competitive ability of beech in the high-montane zones suggests a shift in the leading edge of beech distribution into higher altitudes in East-Central Europe.
机译:气候的长期变化大大影响了欧洲的树木生长和物种分布。在本研究中,FAGUS Sylvatica(L.)和Picea附近的径向生长((L.)喀斯特。西喀尔巴阡山脉。在两次期间,参考期1961-1990和近期1991 - 2012年期间,基于增量核和标准树枝状方法的样品分析了温度和降水变化的树木和降水变化。云杉和山毛榉到气候最近变化的生长响应与高蒙胺区相似,山毛榉的径向增量的改善与云杉相比显着提高。生长反应主要是温度驱动。在亚蒙烷面积中,近期沉淀效果的增加因变暖的负面影响而覆盖,缓解的温度限制对蒙太金属和高蒙尾区的树木生长有明显的支持作用。在不久的将来,由于预期的景观干燥,变暖可能导致山毛榉的径向增量径向增量下降。与此同时,山毛榉在高蒙尾区的竞争能力提高表明山毛榉分布的前缘转变为东部中欧的更高海拔。

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