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DOI | 10.1016/j.quascirev.2019.106087 |
+A 5680-year tree-ring temperature record for southern South America | |
Lara A.; Villalba R.; Urrutia-Jalabert R.; González-Reyes A.; Aravena J.C.; Luckman B.H.; Cuq E.; Rodríguez C.; Wolodarsky-Franke A. | |
发表日期 | 2020 |
ISSN | 0277-3791 |
卷号 | 228 |
英文摘要 | It is widely documented that the Earth's surface temperatures have increased in recent decades. However, temperature increment patterns are not uniform around the globe, showing different or even contrasting trends. Here we present a mean maximum summer temperature record, based on tree-ring widths, over the past 5682 years (3672BC – 2009AD) for southern South America (SSA), covering from mid-Holocene to the present. This is the longest such record for the Southern Hemisphere (SH), and expands available annual proxy climate records for this region in more than 2060 years. Our record explains 49% of the temperature variation, and documents two major warm periods between 3140–2800BC and 70BC – 150AD, which coincide with the lack of evidence of glacier advances in SSA. Recent decades in the reconstruction (1959–2009) show a warming trend that is not exceptional in the context of the last five millennia. The long-term relationship between our temperature reconstruction and a reconstructed total solar irradiance record, with coinciding cycles at 293, 372, 432–434, 512 and 746 years, indicate a persistent influence of solar forcing on centennial climate variability in SSA. At interannual to interdecadal scales, reconstructed temperature is mainly related to the internal climate variability of the Pacific Ocean, including El Niño Southern Oscillation (ENSO) and longer oscillations. Our study reveals the need to characterize regional-scale climate variability and its drivers, which in the context of global-scale processes such as anthropogenic warming, interact to modulate local climate affecting humans and ecosystems. © 2019 The Authors |
英文关键词 | Holocene; Paleoclimatology; South America; Tree-rings |
语种 | 英语 |
scopus关键词 | Atmospheric pressure; Forestry; Holocenes; Internal climate variability; Long-term relationships; Paleoclimatology; South America; Temperature reconstruction; Total solar irradiance; Tree rings; Climatology; El Nino-Southern Oscillation; paleoclimate; paleotemperature; proxy climate record; tree ring; trend analysis; South America |
来源期刊 | Quaternary Science Reviews
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151633 |
作者单位 | Laboratorio de Dendrocronología y Cambio Global, Instituto de Conservación, Biodiversidad y Territorio, Facultad de Ciencias Forestales y Recursos Naturales, Universidad Austral de Chile, Valdivia, Chile; Center for Climate and Resilience Research (CR)2, Santiago, Chile; Fundación Centro de los Bosques Nativos FORECOS, Valdivia, Chile; Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA-CONICET), Mendoza, Argentina; Instituto Forestal (INFOR), Fundo Teja Norte S/N, Valdivia, Chile; Hémera Centro de Observación de la Tierra, Facultad de Ciencias, Universidad Mayor, Santiago, Chile; Centro de Investigación Antártica, Universidad de Magallanes, Punta Arenas, Chile; Department of Geography, University of Western Ontario, London, Ontario, Canada; Cooperativa Calahuala, Valdivia, Chile |
推荐引用方式 GB/T 7714 | Lara A.,Villalba R.,Urrutia-Jalabert R.,et al. +A 5680-year tree-ring temperature record for southern South America[J],2020,228. |
APA | Lara A..,Villalba R..,Urrutia-Jalabert R..,González-Reyes A..,Aravena J.C..,...&Wolodarsky-Franke A..(2020).+A 5680-year tree-ring temperature record for southern South America.Quaternary Science Reviews,228. |
MLA | Lara A.,et al."+A 5680-year tree-ring temperature record for southern South America".Quaternary Science Reviews 228(2020). |
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