DOI: 10.1016/j.quascirev.2015.07.009
Scopus记录号: 2-s2.0-84939802322
论文题名: Southeast African records reveal a coherent shift from high- to low-latitude forcing mechanisms along the east African margin across last glacial-interglacial transition
作者: Chevalier M. ; Chase B.M.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2015
卷: 125 起始页码: 117
结束页码: 130
语种: 英语
英文关键词: Climate reconstruction
; East Africa
; Holocene
; Insolation forcing
; ITCZ
; Palaeoclimatology
; Pollen
; Quaternary
; Southern Africa
Scopus关键词: Atmospheric temperature
; Climate change
; Climatology
; Glacial geology
; Incident solar radiation
; Plants (botany)
; Precipitation (meteorology)
; Rain
; Repair
; Solar radiation
; Surface waters
; Tropics
; Climate reconstruction
; East Africa
; Holocenes
; Insolation forcing
; ITCZ
; Palaeoclimatology
; Pollen
; Quaternary
; Southern Africa
; Oceanography
; glacial-interglacial cycle
; Holocene
; insolation
; Last Glacial-Interglacial
; latitude
; paleoclimate
; pollen
; rainfall
; reconstruction
; sea surface height
; sea surface temperature
; trough
; Indian Ocean
; Southern Africa
英文摘要: Late Quaternary climate variability in the southern African subtropics is still only poorly resolved, with significant complexity and apparent contradictions in the regional dataset. To more effectively interpret and synthesize key regional records, we reanalysed the data from 13 pollen sequences from the summer rainfall zone of South Africa spanning the last 45,000 years, obtaining directly comparable quantitative reconstructions of mean annual temperature and summer rainfall. Temperature reconstructions from across the region provide consistent results, with all sites reflecting trends observed in southwest Indian Ocean sea-surface temperatures in the adjacent Mozambique Channel. Precipitation reconstructions are more heterogeneous, with two distinct subregions being identified. In the northeast, long-term trends in precipitation are determined by sea-surface and continental temperature trends, revealing a positive relationship between temperature and rainfall. This long-term pattern appears to be primarily driven by high northern latitude mechanisms, with direct local insolation being subordinate. Their relative impact reversed during terminal glacial period/early Holocene, at which time direct insolation forcing became the main driver of rainfall variability. Further south, in central South Africa, precipitation variability appears also to be influenced by the latitudinal position of the Southern Hemisphere westerlies, which combine with tropical flow to create tropical-temperate trough, advecting moisture into the interior. In this region, periods of maximum precipitation coincide with periods of elevated SSTs and equatorward expansions of the westerly storm track. This study allows for a fully constrained understanding of climate dynamics along the eastern African margin for the last 45,000 years, linking dynamics to drivers and describing how the climate systems evolved across the last glacial-interglacial transition. © 2015 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59840
Appears in Collections: 过去全球变化的重建
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作者单位: Centre National de la Recherche Scientifique, UMR 5554, Institut des Sciences de l'Evolution de Montpellier, Université de Montpellier, Bat 22, CC061, Place Eugène Bataillon, Montpellier Cedex 5, France
Recommended Citation:
Chevalier M.,Chase B.M.. Southeast African records reveal a coherent shift from high- to low-latitude forcing mechanisms along the east African margin across last glacial-interglacial transition[J]. Quaternary Science Reviews,2015-01-01,125