Timing of the Antarctic cold reversal and the atmospheric CO2increase with respect to the Younger Dryas Event
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Was a change in thermohaline circulation responsible for the Little Ice Age?Late-glacial elevated dust deposition linked to westerly wind shifts in southern South AmericaHolocene Climate Variability in Antarctica Based on 11 Ice-Core Isotopic RecordsA minimum thermodynamic model for the bipolar seesawA premature burial: comments on Grayson and Meltzer's “Requiem for overkill”Multiproxy Record of Late Pleistocene–Holocene Climate and Vegetation Changes from a Peat Bog in PatagoniaMechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula regionThe δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instabilityModelling terrestrial vegetation dynamics and carbon cycling for an abrupt climatic change eventPossible changes of δ18O in precipitation caused by a meltwater event in the North AtlanticThe deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxiaThe spatial extent and dynamics of the Antarctic Cold ReversalImpact of oceanic reorganizations on the ocean carbon cycle and atmospheric carbon dioxide contentPhysical and biogeochemical responses to freshwater-induced thermohaline variability in a zonally averaged ocean modelA critical review of marine sedimentaryδ13Corg-pCO2estimates: New palaeorecords from the South China Sea and a revisit of other low-latitude δ13Corg-pCO2recordsA glacial stage spanning the antarctic cold reversal in torres del paine (51°s), chile, based on preliminary cosmogenic exposure agesLate‐glacial glacier events in southernmost south america: a blend of ‘northern’ and 'southern’ hemispheric climatic signals?Atmospheric CO2 concentration and millennial-scale climate change during the last glacial periodGlacial/interglacial changes in mineral dust and sea-salt records in polar ice cores: Sources, transport, and depositionEvidence for late‐glacial ice dammed lakes in the central strait of magellan and bahía inútil, southernmost south americaThe transition from the Last Glacial Period in inland and near-coastal AntarcticaSouth dials northVariations of Younger Dryas atmospheric radiocarbon explicable without ocean circulation changes
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P2860
Timing of the Antarctic cold reversal and the atmospheric CO2increase with respect to the Younger Dryas Event
description
im November 1997 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 1997
@uk
name
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@en
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@nl
type
label
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@en
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@nl
prefLabel
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@en
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@nl
P2093
P2860
P356
P1476
Timing of the Antarctic cold r ...... ect to the Younger Dryas Event
@en
P2093
A. Dällenbach
A. Indermühle
B. Stauffer
D. Raynaud
J. Chappellaz
J. Schwander
J. Tschumi
J.-M. Barnola
T. Stocker
P2860
P304
P356
10.1029/97GL02658
P407
P577
1997-11-01T00:00:00Z