DOI: 10.5194/cp-9-1645-2013
Scopus记录号: 2-s2.0-84881266122
论文题名: Caspian sea-level changes during the last millennium: Historical and geological evidence from the south Caspian Sea
作者: Beni A.N. ; Lahijani H. ; Harami R.M. ; Arpe K. ; Leroy S.A.G. ; Marriner N. ; Berberian M. ; Andrieu-Ponel V. ; Djamali M. ; Mahboubi A. ; Reimer P.J.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2013
卷: 9, 期: 4 起始页码: 1645
结束页码: 1665
语种: 英语
Scopus关键词: climatology
; geological record
; historical record
; paleoceanography
; paleoclimate
; reconstruction
; sea level change
; Caspian Sea
英文摘要: Historical literature may constitute a valuable source of information to reconstruct sea-level changes. Here, historical documents and geological records have been combined to reconstruct Caspian sea-level (CSL) changes during the last millennium. In addition to a comprehensive literature review, new data from two short sediment cores were obtained from the south-eastern Caspian coast to identify coastal change driven by water-level changes and to compare the results with other geological and historical findings. The overall results indicate a high-stand during the Little Ice Age, up to -21m (and extra rises due to manmade river avulsion), with a -28m low-stand during the Medieval Climate Anomaly, while presently the CSL stands at -26.5 m. A comparison of the CSL curve with other lake systems and proxy records suggests that the main sea-level oscillations are essentially paced by solar irradiance. Although the major controller of the long-term CSL changes is driven by climatological factors, the seismicity of the basin creates local changes in base level. These local base-level changes should be considered in any CSL reconstruction. © Author(s) 2013.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49493
Appears in Collections: 气候变化与战略
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Recommended Citation:
Beni A.N.,Lahijani H.,Harami R.M.,et al. Caspian sea-level changes during the last millennium: Historical and geological evidence from the south Caspian Sea[J]. Climate of the Past,2013-01-01,9(4)