DOI: 10.5194/cp-12-1297-2016
Scopus记录号: 2-s2.0-84973402415
论文题名: 1200 years of warm-season temperature variability in central Scandinavia inferred from tree-ring density
作者: Zhang P. ; Linderholm H.W. ; Gunnarson B.E. ; Bjorklund J. ; Chen D.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2016
卷: 12, 期: 6 起始页码: 1297
结束页码: 1312
语种: 英语
Scopus关键词: algorithm
; high temperature
; Little Ice Age
; Medieval Warm Period
; mountain region
; reconstruction
; seasonal variation
; tree ring
; warming
; Fennoscandia
; Scandinavia
; Pinus sylvestris
英文摘要: Despite the emergence of new high-resolution temperature reconstructions around the world, only a few cover the Medieval Climate Anomaly (MCA). Here we present C-Scan, a new Scots pine tree-ring density-based reconstruction of warm-season (April-September) temperatures for central Scandinavia back to 850 CE, extending the previous reconstruction by 250 years. C-Scan is based on samples collected in a confined mountain region, adjusted for their differences in altitude and local environment, and standardised using the new RSFi algorithm to preserve lowfrequency signals. In C-Scan, the warm peak of MCA occurs ca. 1000-1100 CE, and the Little Ice Age (LIA) between 1550 and 1900 CE. Moreover, during the last millennium the coldest decades are found around 1600 CE, and the warmest 10 and 30 years occur in the most recent century. By comparing C-Scan with other millennium-long temperature reconstructions from Fennoscandia, regional differences in multi-decadal temperature variability, especially during the warm period of the last millennium are revealed. Although these differences could be due to methodological reasons, they may indicate asynchronous warming patterns across Fennoscandia. Further investigation of these regional differences and the reasons and mechanisms behind them are needed. © 2016 Author(s). Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49006
Appears in Collections: 气候变化与战略
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Recommended Citation:
Zhang P.,Linderholm H.W.,Gunnarson B.E.,et al. 1200 years of warm-season temperature variability in central Scandinavia inferred from tree-ring density[J]. Climate of the Past,2016-01-01,12(6)