DOI: 10.1016/j.quascirev.2018.07.003
Scopus记录号: 2-s2.0-85052462960
论文题名: Last glacial maximum glaciers in the Northern Apennines reflect primarily the influence of southerly storm-tracks in the western Mediterranean
作者: Baroni C. ; Guidobaldi G. ; Salvatore M.C. ; Christl M. ; Ivy-Ochs S.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 197 起始页码: 352
结束页码: 367
语种: 英语
英文关键词: Cosmogenic isotopes
; ELA
; Europe
; Glacial geomorphology
; Glaciation
; Italy
; Last Glacial Maximum
; Pleistocene
Scopus关键词: Facings
; Landforms
; Storms
; Cosmogenic isotopes
; Europe
; Glacial geomorphology
; Glaciation
; Italy
; Last Glacial Maximum
; Pleistocene
; Glacial geology
; atmospheric circulation
; geomorphology
; glaciation
; Last Glacial Maximum
; mountain region
; Pleistocene
; storm track
; Alps
; Apennines
; Europe
; Italian Peninsula
; Italy
; Italy
; Mediterranean Region
英文摘要: During the Local Last Glacial Maximum (LLGM), the Northern Apennines hosted more than 100 valley and mountain glaciers covering collectively more than 260 km2. Cosmogenic 10Be exposure ages obtained for the first time along the Apenninic range constrain the age of the LLGM to pre-date ca 21 ka. The estimated volumes of these Late Pleistocene glaciers exceeded 9.1 km3 w.e. Their reconstructed Equilibrium Line Altitudes (ELAs) range from ca. 1200 m a.s.l. for northerly facing compound basin valley glaciers to ca. 1620 m a.s.l. for southerly facing mountain glaciers. Reconstructed ELAs in the western sector of the Northern Apennines were among the lowest recorded for the whole of the Italian peninsula, including the Alps, and also when compared with other mountain chains in the surrounding Mediterranean basin. These probably reflect exceptionally high accumulation rates fed by storm tracks in the western Mediterranean, which in turn has implications for the atmospheric circulation pattern that prevailed in the region at the time. © 2018 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112063
Appears in Collections: 气候减缓与适应
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作者单位: Dipartimento di Scienze della Terra, University of Pisa, Via S. Maria 53 56126, Pisa, Italy; Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche, Pisa, Italy; Laboratory of Ion Beam Physics, ETH Zürich, Switzerland
Recommended Citation:
Baroni C.,Guidobaldi G.,Salvatore M.C.,et al. Last glacial maximum glaciers in the Northern Apennines reflect primarily the influence of southerly storm-tracks in the western Mediterranean[J]. Quaternary Science Reviews,2018-01-01,197