globalchange  > 气候变化与战略
DOI: 10.5194/cp-8-1367-2012
Scopus记录号: 2-s2.0-84871080252
论文题名:
Holocene climate variability in north-eastern Italy: Potential influence of the NAO and solar activity recorded by speleothem data
作者: Scholz D.; Frisia S.; Borsato A.; Spötl C.; Fohlmeister J.; Mudelsee M.; Miorandi R.; Mangini A.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2012
卷: 8, 期:4
起始页码: 1367
结束页码: 1383
语种: 英语
Scopus关键词: cave ; climate variation ; hiatus ; Holocene ; North Atlantic Oscillation ; paleoclimate ; radiocarbon dating ; sapropel ; solar activity ; spectral analysis ; speleothem ; stable isotope ; stalagmite ; uranium series dating ; Italy ; Mediterranean Sea
英文摘要: Here we present high-resolution stable isotope and lamina thickness profiles as well as radiocarbon data for the Holocene stalagmite ER 76 from Grotta di Ernesto (north-eastern Italy), which was dated by combined U-series dating and lamina counting. ER 76 grew between 8 ka (thousands of years before 2000 AD) and today, with a hiatus from 2.6 to 0.4 ka. Data from nine meteorological stations in Trentino show a significant influence of the North Atlantic Oscillation (NAO) on winter temperature and precipitation in the cave region. Spectral analysis of the stable isotope signals of ER 76 reveals significant peaks at periods of 110, 60-70, 40-50, 32-37 and around 25 a. Except for the cycle between 32 and 37 a all periodicities have corresponding peaks in power spectra of solar variability, and the 25-a cycle may correspond to NAO variability. This suggests that climate variability in northern Italy was influenced by both solar activity and the NAO during the Holocene. Six periods of warm winter climate in the cave region were identified. These are centred at 7.9, 7.4, 6.5, 5.5, 4.9 and 3.7 ka, and their duration ranges from 100 to 400 a. The two oldest warm phases coincide with the deposition of sapropel S1 in the Mediterranean Sea indicating that the climate in the cave region was influenced by this prominent pluvial phase in the Mediterranean area. For the younger warm phases it is difficult to establish a supra-regional climate pattern, and some of them may, thus, reflect regional climate variability. This highlights the complexity of regional and supra-regional scale Holocene climate patterns. © Author(s) 2012.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49538
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Recommended Citation:
Scholz D.,Frisia S.,Borsato A.,et al. Holocene climate variability in north-eastern Italy: Potential influence of the NAO and solar activity recorded by speleothem data[J]. Climate of the Past,2012-01-01,8(4)
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