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首页> 外文期刊>Global and planetary change >Evidence of solar activity and El Nino signals in tree rings of Araucaria araucana and A. angustifolia in South America
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Evidence of solar activity and El Nino signals in tree rings of Araucaria araucana and A. angustifolia in South America

机译:南美洲南洋杉和A. angustifolia年轮中太阳活动和厄尔尼诺现象的证据

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摘要

Tree rings reveal climatic variations through years, but also the effect of solar activity in influencing the climate on a large scale. In order to investigate the role of solar cycles non climatic variability and to analyse their influences on tree growth, we focused on tree-ring chronologies of Araucaria angustifolia and Araucaria araucana in four study areas: Irati and Curitiba in Brazil, Caviahue in Chile, and Tolhuaca in Argentina. We obtained an average tree-ring chronology of 218, 117, 439, and 849 years for these areas, respectively. Particularly, the older chronologies also included the period of the Maunder and Dalton minima. To identify periodicities and trends observable in tree growth, the time series were analysed using spectral, wavelet and cross-wavelet techniques. Analysis based on the Multitaper method of annual growth rates identified 2 cycles with periodicities of 11 (Schwebe cycle) and 5.5 years (second harmonic of Schwebe cycle). In the Chilean and Argentinian sites, significant agreement between the time series of tree rings and the 11-year solar cycle was found during the periods of maximum solar activity. Results also showed oscillation with periods of 2-7 years, probably induced by local environmental variations, and possibly also related to the El-Nino events. Moreover, the Morlet complex wavelet analysis was applied to study the most relevant variability factors affecting tree-ring time series. Finally, we applied the cross-wavelet spectral analysis to evaluate the time lags between tree-ring and sunspot-number time series, as well as for the interaction between tree rings, the Southern Oscillation Index (SOI) and temperature and precipitation. Trees sampled in Chile and Argentina showed more evident responses of fluctuations in tree-ring time series to the variations of short and long periodicities in comparison with the Brazilian ones. These results provided new evidence on the solar activity-climate pattern-tree ring connections over centuries. (C) 2016 Elsevier B.V. All rights reserved.
机译:年轮揭示了多年来的气候变化,但也揭示了太阳活动在很大程度上影响气候的作用。为了研究太阳周期非气候变化的作用并分析其对树木生长的影响,我们集中研究了四个研究区域中的南洋杉和南洋杉的年轮年表:巴西的Irati和库里蒂巴,智利的Caviahue和阿根廷的托尔瓦卡。对于这些区域,我们分别获得了218年,117年,439年和849年的平均年轮年表。特别是,较早的年代还包括Maunder和Dalton极小时期。为了确定树木生长中可观察到的周期性和趋势,使用光谱,小波和交叉小波技术分析了时间序列。基于Multitaper年增长率的分析确定了2个周期,周期分别为11(Schwebe周期)和5.5年(Schwebe周期的二次谐波)。在智利和阿根廷的站点中,在太阳活动最多的时期,树木年轮的时间序列与11年太阳周期之间存在显着一致性。结果还显示,振荡周期为2-7年,可能是由当地环境变化引起的,也可能与El-Nino事件有关。此外,使用Morlet复数小波分析来研究影响树木年轮时间序列的最相关变异性因素。最后,我们应用交叉小波谱分析来评估树轮与黑子数时间序列之间的时滞,以及树轮,南方涛动指数(SOI)与温度和降水之间的相互作用。与巴西的树木相比,在智利和阿根廷采样的树木显示出树木年轮时间序列波动对短期和长期周期性变化的更明显的响应。这些结果提供了几个世纪以来太阳活动-气候模式-树环连接的新证据。 (C)2016 Elsevier B.V.保留所有权利。

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