DOI: 10.1016/j.quascirev.2015.10.009
Scopus记录号: 2-s2.0-84944881419
论文题名: Major storm periods and climate forcing in the Western Mediterranean during the Late Holocene
作者: Degeai J.-P. ; Devillers B. ; Dezileau L. ; Oueslati H. ; Bony G.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2015
卷: 129 起始页码: 37
结束页码: 56
语种: 英语
英文关键词: Climate forcing
; Lagoonal sequence
; Late Holocene
; Solar activity
; Storminess activity
; Western Mediterranean
Scopus关键词: Geochemistry
; Magnetic susceptibility
; Solar energy
; Spectrum analysis
; Climate forcings
; Lagoonal sequence
; Late Holocene
; Solar activity
; Western Mediterranean
; Storms
英文摘要: Big storm events represent a major risk for populations and infrastructures settled on coastal lowlands. In the Western Mediterranean, where human societies colonized and occupied the coastal areas since the Ancient times, the variability of storm activity for the past three millennia was investigated with a multi-proxy sedimentological and geochemical study from a lagoonal sequence. Mappings of the geochemistry and magnetic susceptibility of detrital sources in the watershed of the lagoon and from the coastal barriers were undertaken in order to track the terrestrial or coastal/marine origin of sediments deposited into the lagoon. The multi-proxy analysis shows that coarser material, low magnetic susceptibility, and high strontium content characterize the sedimentological signature of the paleostorm levels identified in the lagoonal sequence. A comparison with North Atlantic and Western Mediterranean paleoclimate proxies shows that the phases of high storm activity occurred during cold periods, suggesting a climatically-controlled mechanism for the occurrence of these storm periods. Besides, an in-phase storm activity pattern is found between the Western Mediterranean and Northern Europe. Spectral analyses performed on the Sr content revealed a new 270-year solar-driven pattern of storm cyclicity. For the last 3000 years, this 270-year cycle defines a succession of ten major storm periods (SP) with a mean duration of 96 ± 54 yr. Periods of higher storm activity are recorded from >680 to 560 cal yr BC (SP10, end of the Iron Age Cold Period), from 140 to 820 cal yr AD (SP7 to SP5) with a climax of storminess between 400 and 800 cal yr AD (Dark Ages Cold Period), and from 1230 to >1800 cal yr AD (SP3 to SP1, Little Ice Age). Periods of low storm activity occurred from 560 cal yr BC to 140 cal yr AD (SP9 and SP8, Roman Warm Period) and from 820 to 1230 cal yr AD (SP4, Medieval Warm Period). © 2015 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59769
Appears in Collections: 过去全球变化的重建
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作者单位: CNRS UMR5140 ASM, Université Montpellier III, MCC, Lattes, France; Université de Montpellier, Géosciences UMR5243, Montpellier, France
Recommended Citation:
Degeai J.-P.,Devillers B.,Dezileau L.,et al. Major storm periods and climate forcing in the Western Mediterranean during the Late Holocene[J]. Quaternary Science Reviews,2015-01-01,129