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Age-dependent tree-ring growth responses of Schrenk spruce (Picea schrenkiana) to climate-A case study in the Tianshan Mountain, China

机译:雪兰克云杉(Picea schrenkiana)对气候的年龄依赖性树轮生长响应-以天山为例

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For both its climatic and ecological importance, Schrenk spruce (Picea schrenkiana) is a crucial tree species living at mid-altitude on the western area of the Tianshan Mountains. It plays a key role on understanding climatic change in the Tianshan Mountains in the past 500 years. However, whether the relationship between tree growth and limiting climate factors is stable over time is still not well-known. In this study, standard and residual chronologies of four 100-year age classes (AC1 < 110a, 110a < AC2 < 210a, 210a < AC3 < 310a and AC4 > 310a) were established for detecting divergence in climate-growth relationships as well as comparing low-frequency and high-frequency variations. The results show that climate can account fora high amount of variance in tree-ring width and higher climate sensitivity was detected in younger trees. Younger trees (<210a) exhibit significantly negative growth responses to mean monthly air temperature of previous June and positive relationship with total monthly precipitation of current April and May, while mean monthly air temperature of current March may inhibit growth of older trees (>210a). Tree-ring chronology statistics and response function reveal that the age-growth patterns are non-monotonic. Our results together with previous studies demonstrate that the age effects on tree-ring growth-climate response is attributed to a combination of genetic characteristics and site microclimate, which suggests that it is necessary to consider both age-dependent and species-specific climate responses when using tree-ring measurements as a proxy for valid climate reconstructions
机译:由于其在气候和生态方面的重要性,Schrenk云杉(Picea schrenkiana)是一种重要的树种,生活在天山西部地区的中海拔地区。它在了解过去500年来天山的气候变化中起着关键作用。但是,树木生长与限制气候因素之间的关系是否随着时间推移而保持稳定仍是未知的。在这项研究中,建立了四个100年年龄类别(AC1 <110a,110a 310a)的标准和剩余年表,以检测气候-增长关系的差异并进行比较低频和高频变化。结果表明,气候可以解释树木年轮宽度的大量变化,并且在年轻树木中检测到较高的气候敏感性。较年轻的树(<210a)对前六月的平均月气温表现出显着的负响应,并且与当前四月和五月的总月降水量呈正相关,而当前三月的平均月气温可能会抑制较老的树(> 210a)的生长。树年轮年代统计和响应函数表明年龄增长模式是非单调的。我们的结果以及以前的研究表明,年龄对树轮生长-气候响应的影响归因于遗传特征和站点小气候的结合,这表明有必要在考虑树木年龄和特定物种的气候响应时使用树轮测量作为有效气候重建的代理

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