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首页> 外文期刊>Canadian Journal of Forest Research >Tree-growth response to climatic variability in two climatically contrasting treeline ecotone areas, central Himalaya, Nepal
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Tree-growth response to climatic variability in two climatically contrasting treeline ecotone areas, central Himalaya, Nepal

机译:尼泊尔喜马拉雅山中部两个气候形成鲜明对比的生态交错带地区,树木生长对气候变异的响应

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摘要

Tree growth at the treeline ecotone is known to be sensitive to climate variability and is thus considered to be a worldwide biomonitor of climate change. However, our understanding of within-region variation in growth responses through space and time is limited. A dry south-facing slope dominated by Pinus wallichiana A. B. Jacks. and a wet north-facing slope dominated by Abies spectabilis (D. Don) Spach in Nepal, central Himalaya, were used to analyze the intersite (i.e., dry vs. wet sites) and intrasite (i.e., treeline vs. forest line elevations) tree-growth relationships, as well as response to monthly and seasonal temperature and precipitation at annual and bidecadal time scales. At both study sites and at two elevations within each site, growth can be strongly affected by growing-season and nongrowing-season factors; however, there are inconsistencies in terms of the climate-growth relationship across space and over time. At the dry site, only a weak positive growth response to summer temperature is observed. At both sites, there is a negative growth response to winter precipitation at both high and low elevations, and this response is markedly independent of the summer and winter temperature trends of the respective site. At the wet site, growth at the higher elevation is negatively correlated to the early summer temperature, whereas a positive growth response to spring precipitation is observed at the lower elevation, indicating a possible drought effect. The results illustrate how different climatic drivers may govern tree-growth responses both between sites with contrasting climates within a region and along elevational gradients within the treeline ecotone. This underlines the need for multiscale studies and a focus on multiple climate variables when analyzing treeline ecotone responses to climate change.
机译:众所周知,树线过渡带的树木生长对气候变化敏感,因此被认为是全球气候变化的生物监测者。但是,我们对区域响应随时间和空间变化的区域内变化的理解是有限的。一个以Pinus wallichiana A. B. Jacks为主的干燥的朝南斜坡。以及在喜马拉雅山中部尼泊尔的一个以北冷杉(Abies spectabilis(D. Don)Spach)为主的朝北湿坡上,用于分析站点间(即干旱与湿地)和站点内(即林线与森林线的海拔)树与树之间的关系,以及在年度和双峰时间尺度下对月度和季节温度和降水的响应。在两个研究地点以及每个地点内的两个海拔高度,生长都会受到季节和非季节因素的强烈影响。但是,跨空间和随时间变化的气候-增长关系存在不一致之处。在干燥的地方,仅观察到对夏季温度的弱正生长响应。在两个地点,高海拔和低海拔都对冬季降水有负增长响应,并且该响应明显独立于各个站点的夏季和冬季温度趋势。在湿地,高海拔地区的生长与初夏温度呈负相关,而在较低海拔地区观察到对春季降水的正增长响应,表明可能存在干旱效应。结果表明,不同的气候驱动因素可能如何控制区域之间气候不同的站点之间以及沿树线过渡带内的海拔梯度的树木生长响应。这强调了在分析树线过渡带对气候变化的响应时需要进行多尺度研究并关注多个气候变量。

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