air temperature
; climate modeling
; cooling
; deep water
; estimation method
; Heinrich event
; Holocene
; last deglaciation
; Last Glacial Maximum
; latitude
; meridional circulation
; protactinium
; proxy climate record
; qualitative analysis
; radiocarbon dating
; reconstruction
; Atlantic Ocean
Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstr. 5, 3012 Bern, Switzerland; Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland; Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research, Spanish Council for Scientific Research, 08034 Barcelona, Spain; Climate Change Research Centre, Centre of Excellence, University of New SouthWales, Sydney, NSW 2052, Australia; IPRC, University of Hawaii, Honolulu, HI 96822, United States
Recommended Citation:
Ritz S.P.,Stocker T.F.,Grimalt J.O.,et al. Estimated strength of the Atlantic overturning circulation during the last deglaciation[J]. Nature Geoscience,2013-01-01,6(3)