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NorthGRIP ice-core record of major ions measured using ion chromatography cov...
Ion concentration data was obtained from the NGRIP1 ice core drilled in 1996 and 1997. NGRIP1 camp position 75.1N, 42.32W. All samples were cut and decontaminated using a... -
Ice thickness data Weißseespitze/Austria
Ice thickness data were recorded at Weißseespitze (3500 m) in the Ötztal Alps/Austria during the FWF project Cold Ice, P 29256-N36. The ice thickness was measured with ground... -
WAIS Divide Ice-Core Volcanic Sulfate from 12.68 to 13.20 ka BP
Annual volcanic sulfate mass deposition rates from the West Antarctic Ice Sheet (WAIS) Divide ice core project for the time period 12.68-13.20 ka BP on the annual-layer counted... -
Sulfate concentration and sulfur isotope data from Greenland TUNU2013 ice-cor...
Sulfate concentration and triple sulfur isotope (32S, 33S, 34S) data measured in TUNU2013 ice-core samples and calculated background-corrected isotope composition (Gabriel et... -
δO2/N2 from EPICA Dome C ice core (Antarctica) (0-800 ka)
This dataset has no description
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δ18O of O2 from EPICA Dome C ice core (Antarctica) (0-800 ka)
This dataset has no description
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Age model output of ice core Skytrain Ice Rise
Age model derived using Paleochrono program using fixed tiepoints described in the paper. Our recommended ice age scale uses ALC age until 1337 a bp and Paleochrono for all... -
Non-sea-salt magnesium of ice core Skytrain Ice Rise
nssMg determined by inductively coupled plasma mass spectrometry (Agilent 7700x ICP-MS) on meltwater from a continuous flow melt device. -
Methane concentrations of ice core Skytrain Ice Rise
Continuous CH4 determined by cavity ringdown spectroscopy (Picarro G2301 CRDS) on air separated from meltwater from a continuous flow melt device. -
Summary of Bayesian onset detection algorithm for abrupt warming transitions ...
Summary statistics of posterior marginal distribution of the onset of abrupt warming transitions located in the last glacial age of the NGRIP record, based on both the d18O and... -
Summary of Bayesian onset detection algorithm for abrupt warming transitions ...
Summary statistics of posterior marginal distribution of the onset of abrupt warming transitions located in the last glacial age of the NGRIP record, based on both the d18O and... -
Gas properties in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Gas properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Properties of ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice surface measurements from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice age uncertainty in ice cores from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Temperature and accumulation rate in ice cores from Larsen blue ice area, Eas...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CO2 in ice cores at core depth 1.95 m from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CO2 in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply...