Antarctic sea ice control on ocean circulation in present and glacial climates
about
Precise interpolar phasing of abrupt climate change during the last ice age.Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes.Sea-ice transport driving Southern Ocean salinity and its recent trends.Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2Evolution of South Atlantic density and chemical stratification across the last deglaciation.Radiocarbon constraints on the extent and evolution of the South Pacific glacial carbon poolGlacial ocean circulation and stratification explained by reduced atmospheric temperature.High-latitude ocean ventilation and its role in Earth's climate transitions.Radiocarbon evidence for enhanced respired carbon storage in the Atlantic at the Last Glacial MaximumSynchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.North Atlantic Deep Water Production during the Last Glacial Maximum.Mean global ocean temperatures during the last glacial transition.Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials.Abyssal ocean overturning shaped by seafloor distribution.Enhanced ocean-atmosphere carbon partitioning via the carbonate counter pump during the last deglacial.Hemispheric sea ice distribution sets the glacial tempoOpening the window to the Southern Ocean: The role of jet dynamicsEddy saturation and frictional control of the Antarctic Circumpolar CurrentThe impact of Southern Ocean residual upwelling on atmospheric CO2 on centennial and millennial timescalesEvolution of the stable carbon isotope composition of atmospheric CO2over the last glacial cycleA lower limit to atmospheric CO2 concentrations over the past 800,000 yearsCoherent Response of Antarctic Intermediate Water and Atlantic Meridional Overturning Circulation During the Last Deglaciation: Reconciling Contrasting Neodymium Isotope Reconstructions From the Tropical AtlanticEvolution of the deep Atlantic water masses since the last glacial maximum based on a transient run of NCAR-CCSM3Sequestration of carbon in the deep Atlantic during the last glaciationAntarctic density stratification and the strength of the circumpolar current during the Last Glacial MaximumNeodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific OceanOceanography: What goes down must come upIncursions of southern-sourced water into the deep North Atlantic during late Pliocene glacial intensification
P2860
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P2860
Antarctic sea ice control on ocean circulation in present and glacial climates
description
2014 nî lūn-bûn
@nan
2014 թուականի Յունիսին հրատարակուած գիտական յօդուած
@hyw
2014 թվականի հունիսին հրատարակված գիտական հոդված
@hy
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
name
Antarctic sea ice control on ocean circulation in present and glacial climates
@ast
Antarctic sea ice control on ocean circulation in present and glacial climates
@en
type
label
Antarctic sea ice control on ocean circulation in present and glacial climates
@ast
Antarctic sea ice control on ocean circulation in present and glacial climates
@en
prefLabel
Antarctic sea ice control on ocean circulation in present and glacial climates
@ast
Antarctic sea ice control on ocean circulation in present and glacial climates
@en
P2093
P2860
P356
P1476
Antarctic sea ice control on ocean circulation in present and glacial climates
@en
P2093
Andrew F Thompson
Andrew L Stewart
Malte F Jansen
Raffaele Ferrari
P2860
P304
P356
10.1073/PNAS.1323922111
P407
P577
2014-06-02T00:00:00Z