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DOI10.5194/tc-15-1157-2021
The case of a southern European glacier which survived Roman and medieval warm periods but is disappearing under recent warming
Moreno A.; Bartolomé M.; Ignacio López-Moreno J.; Pey J.; Pablo Corella J.; García-Orellana J.; Sancho C.; Leunda M.; Gil-Romera G.; González-Sampériz P.; Pérez-Mejías C.; Navarro F.; Otero-García J.; Lapazaran J.; Alonso-González E.; Cid C.; López-Martínez J.; Oliva-Urcia B.; Faria S.H.; Sierra M.J.; Millán R.; Querol X.; Alastuey A.; García-Ruíz J.M.
发表日期2021
ISSN19940416
起始页码1157
结束页码1172
卷号15期号:2
英文摘要Mountain glaciers have generally experienced an accelerated retreat over the last 3 decades as a rapid response to current global warming. However, the response to previous warm periods in the Holocene is not well-described for glaciers of the southern Europe mountain ranges, such as the Pyrenees. The situation during the Medieval Climate Anomaly (900-1300 CE) is particularly relevant since it is not certain whether the southern European glaciers just experienced significant ice loss or whether they actually disappeared. We present here the first chronological study of a glacier located in the Central Pyrenees (NE Spain), Monte Perdido Glacier (MPG), carried out by different radiochronological techniques and a comparison with geochemical proxies from neighbouring palaeoclimate records. The chronological model evidences that the glacier persisted during the Roman period and the Medieval Climate Anomaly. The apparent absence of ice in the past ∼ 600 years suggests that any ice accumulated during the Little Ice Age has since ablated. This interpretation is supported by measured concentrations of anthropogenic metals, including Zn, Se, Cd, Hg and Pb, which have concentrations well below those typical of industrial-age ice measured at other glaciers in Europe. This study strengthens the general understanding that warming of the past few decades has been exceptional for the past 2 millennia. © Author(s) 2021.
英文关键词climate modeling; global warming; Holocene; Little Ice Age; Medieval Warm Period; mountain region; paleoclimate; Pyrenees
语种英语
来源期刊Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202387
作者单位Departamento de Procesos Geoambientales y Cambio Global, Instituto Pirenaico de Ecología - CSIC, Zaragoza, Spain; Departamento de Geología, Museo de Ciencias Naturales - CSIC, Madrid, Spain; Fundación Agencia Aragonesa para la Investigación y el Desarrollo, ARAID, Zaragoza, Spain; CIEMAT - Environmental Department (DMA), Avenida Complutense 40, Madrid, Spain; Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona, Barcelona, Spain; Departament de Física, Universitat Autònoma de Barcelona, Barcelona, Spain; Department of Earth Sciences, University of Zaragoza, Zaragoza, Spain; Institute of Plant Sciences, Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland; Swiss Federal Research Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, Switzerland; Ecology Research Group, Department of Biology, Philipps University of Marburg, Marburg, Germany; Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, China; Departamento de ...
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GB/T 7714
Moreno A.,Bartolomé M.,Ignacio López-Moreno J.,et al. The case of a southern European glacier which survived Roman and medieval warm periods but is disappearing under recent warming[J],2021,15(2).
APA Moreno A..,Bartolomé M..,Ignacio López-Moreno J..,Pey J..,Pablo Corella J..,...&García-Ruíz J.M..(2021).The case of a southern European glacier which survived Roman and medieval warm periods but is disappearing under recent warming.Cryosphere,15(2).
MLA Moreno A.,et al."The case of a southern European glacier which survived Roman and medieval warm periods but is disappearing under recent warming".Cryosphere 15.2(2021).
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