DOI: 10.1016/j.quascirev.2014.06.028
Scopus记录号: 2-s2.0-84924424232
论文题名: A brief history of climate e the northern seas from the last Glacial Maximum to global warming
作者: Eldevik T. ; Risebrobakken B. ; Bjune A.E. ; Andersson C. ; Birks H.J.B. ; Dokken T.M. ; Drange H. ; Glessmer M.S. ; Li C. ; Nilsen J.E.O. ; Otterå O.H. ; Richter K. ; Skagseth O.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2014
卷: 106, 期: 1 起始页码: 225
结束页码: 246
语种: 英语
英文关键词: Climate
; Climate model
; LGM-to-future
; Marine
; North atlantic, nordic seas, and arctic
; Observations
; Reconstruction
; Temperature
; Terrestrial
; Thermohaline circulation
Scopus关键词: Climate change
; Climatology
; Glacial geology
; Global warming
; Image reconstruction
; Ocean currents
; Temperature
; Climate
; LGM-to-future
; Marine
; Nordic seas
; Observations
; Terrestrial
; Thermohaline circulations
; Climate models
; climate modeling
; global warming
; Last Glacial Maximum
; paleoclimate
; proxy climate record
; thermohaline circulation
; time series
; twenty first century
; Arctic Ocean
; Norwegian Sea
英文摘要: The understanding of climate and climate change is fundamentally concerned with two things: a welldefined and sufficiently complete climate record to be explained, for example of observed temperature, and a relevant mechanistic framework for making closed and consistent inferences concerning causeand-effect. This is the case for understanding observed climate, as it is the case for historical climate as reconstructed from proxy data and future climate as projected by models. The present study offers a holistic description of northern maritime climate e from the Last Glacial Maximum through to the projected global warming of the 21st century e in this context. It includes the compilation of the most complete temperature record for Norway and the Norwegian Sea to date based on the synthesis of available terrestrial and marine paleoclimate reconstructions into continuous times series, and their continuation into modern and future climate with the instrumental record and a model projection. The scientific literature on a variable northern climate is reviewed against this background, and with a particular emphasis on the role of the Norwegian Atlantic Current e the Gulf Stream's extension towards the Arctic. This includes the introduction of an explicit and relatively simple diagnostic relation to quantify the change in ocean circulation consistent with reconstructed ocean temperatures. It is found that maritime climate and the strength of the Norwegian Atlantic Current are closely related throughout the record. The nature of the relation is however qualitatively different as one progresses from the past, through the present, and into the future. © 2014 The Authors. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60421
Appears in Collections: 过去全球变化的重建
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作者单位: Geophysical Institute, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway; Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway; Department of Biology, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway; Nansen Environmental and Remote Sensing Center, Bjerknes Centre for Climate Research, Bergen, Norway; Institute for Meteorology and Geophysics, University of Innsbruck, Innsbruck, Austria; Institute of Marine Research, Bjerknes Centre for Climate Research, Bergen, Norway; Environmental Change Research Centre, University College London, London, United Kingdom; School of Geography and the Environment, University of Oxford, Oxford, United Kingdom
Recommended Citation:
Eldevik T.,Risebrobakken B.,Bjune A.E.,et al. A brief history of climate e the northern seas from the last Glacial Maximum to global warming[J]. Quaternary Science Reviews,2014-01-01,106(1)