Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings
about
Validation of climate model-inferred regional temperature change for late-glacial EuropeSea-level constraints on the amplitude and source distribution of Meltwater Pulse 1AAbrupt glacial climate shifts controlled by ice sheet changes.Gradual onset and recovery of the Younger Dryas abrupt climate event in the tropics.Abrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise.Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial TerminationDeglacial rapid sea level rises caused by ice-sheet saddle collapses.Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.Centennial-scale Holocene climate variations amplified by Antarctic Ice Sheet discharge.Oyster reef die-offs in stratigraphic record of Corpus Christi Bay, Texas, possibly caused by drought-driven extreme salinity changesStrong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger DryasAssessing divergent SST behavior during the last 21 ka derived from alkenones andG. ruber-Mg/Ca in the equatorial PacificOcean circulation reconstructions fromεNd: A model-based feasibility studyEstimated strength of the Atlantic overturning circulation during the last deglaciationPoorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison studyImpact of oceanic circulation changes on atmosphericδ13CO2Toward explaining the Holocene carbon dioxide and carbon isotope records: Results from transient ocean carbon cycle-climate simulationsCan we use ice sheet reconstructions to constrain meltwater for deglacial simulations?Evaluation of PMIP2 and PMIP3 simulations of mid-Holocene climate in the Indo-Pacific, Australasian and Southern Ocean regionsCollapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation21,000 Years of Ethiopian African monsoon variability recorded in sediments of the western Nile deep-sea fan
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Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings
description
im Mai 2011 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в травні 2011
@uk
name
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@en
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@nl
type
label
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@en
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@nl
prefLabel
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@en
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@nl
P1476
Deconstructing the Last Glacia ...... ial and orbital-scale forcings
@en
P2093
L. Menviel
O. Elison Timm
P304
P356
10.1016/J.QUASCIREV.2011.02.005
P577
2011-05-01T00:00:00Z