The deglacial evolution of North Atlantic deep convection.
about
Validation of climate model-inferred regional temperature change for late-glacial EuropePaleoclimate. Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming.Greenland temperature response to climate forcing during the last deglaciation.Hydrological change in Southern Europe responding to increasing North Atlantic overturning during Greenland Stadial 1Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific.Episodic release of CO2 from the high-latitude North Atlantic Ocean during the last 135 kyr.Radiocarbon evidence for alternating northern and southern sources of ventilation of the deep Atlantic carbon pool during the last deglaciation.Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.North Atlantic forcing of moisture delivery to Europe throughout the Holocene.The Southern Ocean's role in carbon exchange during the last deglaciation.PALEOCEANOGRAPHY. A warm and poorly ventilated deep Arctic Mediterranean during the last glacial period.Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago.Atmospheric science. Refining the radiocarbon time scale.Ice sheet sources of sea level rise and freshwater discharge during the last deglaciationAbrupt changes in deep Atlantic circulation during the transition to full glacial conditionsAtmospheric Δ14C reduction in simulations of Atlantic overturning circulation shutdownA Note on Reporting of Reservoir 14C Disequilibria and Age OffsetsMarine radiocarbon reservoir age simulations for the past 50,000 yearsNorth Atlantic ventilation of “southern-sourced” deep water in the glacial oceanCalibration and application of B/Ca, Cd/Ca, and δ11B inNeogloboquadrina pachyderma(sinistral) to constrain CO2uptake in the subpolar North Atlantic during the last deglaciationTiming of Deglacial AMOC Variability From a High-Resolution Seawater Cadmium ReconstructionDependence of abrupt Atlantic meridional ocean circulation changes on climate background statesStrong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger DryasPoorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison studySouthwest Atlantic water mass evolution during the last deglaciationDansgaard-Oeschger cycles: Interactions between ocean and sea ice intrinsic to the Nordic seasVariability in mid-depth ventilation of the western Atlantic Ocean during the last deglaciationBrine formation recorded by stable isotopes of Recent benthic foraminifera in Storfjorden, Svalbard: palaeoceanographical implicationsVentilation history of Nordic Seas overflows during the last (de)glacial period revealed by species-specific benthic foraminiferal14C datesDynamic intermediate ocean circulation in the North Atlantic during Heinrich Stadial 1: A radiocarbon and neodymium isotope perspectiveThe silicon cycle impacted by past ice sheets
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P2860
The deglacial evolution of North Atlantic deep convection.
description
2011 nî lūn-bûn
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2011年の論文
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2011年学术文章
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2011年学术文章
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2011年学术文章
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2011年学术文章
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2011年学术文章
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name
The deglacial evolution of North Atlantic deep convection.
@en
The deglacial evolution of North Atlantic deep convection.
@nl
type
label
The deglacial evolution of North Atlantic deep convection.
@en
The deglacial evolution of North Atlantic deep convection.
@nl
prefLabel
The deglacial evolution of North Atlantic deep convection.
@en
The deglacial evolution of North Atlantic deep convection.
@nl
P2093
P2860
P356
P1433
P1476
The deglacial evolution of North Atlantic deep convection
@en
P2093
David J R Thornalley
Henry Elderfield
Wallace S Broecker
P2860
P304
P356
10.1126/SCIENCE.1196812
P407
P577
2011-01-01T00:00:00Z