Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores
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Wildfire responses to abrupt climate change in North AmericaHolocene elephant seal distribution implies warmer-than-present climate in the Ross Sea.Paleoclimate. Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming.Gradual onset and recovery of the Younger Dryas abrupt climate event in the tropics.The influence of historical climate changes on Southern Ocean marine predator populations: a comparative analysis.Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial TerminationHolocene peatland and ice-core data constraints on the timing and magnitude of CO2 emissions from past land use.Southern Annular Mode-like changes in southwestern Patagonia at centennial timescales over the last three millennia.Volcanic influence on centennial to millennial Holocene Greenland temperature changeEvolution of South Atlantic density and chemical stratification across the last deglaciation.Holocene Southern Ocean surface temperature variability west of the Antarctic Peninsula.Carbon isotope discrimination in leaves of the broad-leaved paperbark tree, Melaleuca quinquenervia, as a tool for quantifying past tropical and subtropical rainfall.Holocene sea ice variability driven by wind and polynya efficiency in the Ross Sea.Carbon storage and potential methane production in the Hudson Bay Lowlands since mid-Holocene peat initiation.Atmospheric CO2 effect on stable carbon isotope composition of terrestrial fossil archives.Deglaciation and glacial erosion: A joint control on magma productivity by continental unloadingClimatic control of the biomass-burning decline in the Americas after ad 1500Antarctic Zone nutrient conditions during the last two glacial cyclesMid-Holocene monsoons: a multi-model analysis of the inter-hemispheric differences in the responses to orbital forcing and ocean feedbacksPollen-climate reconstruction from northern South Island, New Zealand (41°S), reveals varying high- and low-latitude teleconnections over the last 16 000 yearsPeatlands and Their Role in the Global Carbon CycleEvolution of the stable carbon isotope composition of atmospheric CO2over the last glacial cycleHistorical greenhouse gas concentrations for climate modelling (CMIP6)Vegetation and climate change during Marine Isotope Stage 3 in ChinaA State-Dependent Quantification of Climate Sensitivity Based on Paleodata of the Last 2.1 Million YearsComment on “Magnetic effect on CO2solubility in seawater: A possible link between geomagnetic field variations and climate” by Alexander Pazur and Michael WinklhoferA model-based interpretation of low-frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric Δ14CSouthwest Atlantic water mass evolution during the last deglaciationEurope on fire three thousand years ago: Arson or climate?Paleoceanographic changes and calcium carbonate dissolution in the central Fram Strait during the last 20 kaVariability of 14C reservoir age and air–sea flux of CO2 in the Peru–Chile upwelling region during the past 12,000 yearsHolocene carbon cycle dynamics
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Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores
description
article
@en
im Juli 2004 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в липні 2004
@uk
name
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@en
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@nl
type
label
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@en
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@nl
prefLabel
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@en
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@nl
P2093
P50
P1476
Evidence for substantial accum ...... Dome, Dome C and DML ice cores
@en
P2093
Bernhard Stauffer
Blandine Bellier
David L Morse
Dominique Raynaud
Eric Monnin
Jakob Schwander
Jean-Marc Barnola
Thomas F Stocker
Urs Siegenthaler
P356
10.1016/J.EPSL.2004.05.007
P407
P577
2004-07-01T00:00:00Z