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Chronology for the EDML ice core from Dronning Maud Land, Antarctica, over th...
A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice... -
Methane and stable isotope record of ice core EDML from Dronning Maud Land, A...
Precise knowledge of the phase relationship between climate changes in the two hemispheres is a key for understanding the Earth's climate dynamics. For the last glacial period,... -
Evaluation of the segmentation performance of air hydrates from microphotogra...
In the deeper part of polar ice sheets, air hydrates are the primary air inclusions. They trap most of the ancient air molecules used for paleoclimatic reconstructions in their... -
Hand-labeled ground truth images of ice thick section microphotographs of the...
In the deeper part of polar ice sheets, air hydrates are the primary air inclusions. They trap most of the ancient air molecules used for paleoclimatic reconstructions in their... -
Summary of air hydrate properties of the EDML ice core
In the deeper part of polar ice sheets, air hydrates are the primary air inclusions. They trap most of the ancient air molecules used for paleoclimatic reconstructions in their... -
Raw data of air hydrate properties of the EDML ice core
In the deeper part of polar ice sheets, air hydrates are the primary air inclusions. They trap most of the ancient air molecules used for paleoclimatic reconstructions in their... -
High-Resolution profiles of stable water isotopes (d18O, dD) analyzed in 201...
Snow-cores KF13, KF14, KF15, KF16, KF17, and KF18 continuously analyzed by Continuous Flow Analysis between April and October 2019 at the Alfred-Wegener-Institut... -
Discrete profiles of stable water isotopes (d18O, dD) measured in 2019 and sa...
Discrete samples at 22mm depth-resolution for snow-cores KF13, KF14, KF15, KF16, analyzed in 2019 at the Alfred-Wegener-Institut Helmholtz-Zentrum für Polar-und Meeresforschung,... -
Local snow dunes / sastrugi heights across the plateau of Dronning Maud Land,...
Local snow surface heights were sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station. They were used to quantify surface roughness and its relation to... -
Discrete profiles of stable water isotopes (d18O, dD) measured in 2015 and sa...
Discrete samples (22mm depth-resolution) for snow-cores KF13, KF14, KF15, KF16, KF17, KF18, analyzed in 2015 at the Alfred-Wegener-Institut Helmholtz-Zentrum für Polar-und... -
Discrete profiles of stable water isotopes (d18O, dD) measured in 2019 and sa...
Discrete samples at 22mm depth-resolution for snow-cores KF13, KF14, KF15, KF16, and 33mm depth-resolution for snow-core KF20, analyzed in 2019 at the Alfred-Wegener-Institut... -
High-Resolution profiles of stable water isotopes (d18O, dD) analyzed in 2019...
Snow-cores KF13, KF14, KF15, KF16, KF17, KF18, and KF20 continuously analyzed by Continuous Flow Analysis between April and October 2019 at the Alfred-Wegener-Institut... -
Condensation particle concentrations at Kohnen in January 2016
This dataset has no description
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Condensation particle concentrations at Kohnen in January 2015
This dataset has no description
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High-resolution sulfur isotopic composition measurements of volcanic sulfate ...
Multiple peaks in sulfate concentration in ice cores have been identified as potential candidates for the ~74 ka Toba supereruption. The sulfur isotopic composition of sulfate... -
Year-round chemical aerosol records at Kohnen, Antarctica obtained by automat...
Aimed at year-round recording of the chemical aerosol composition in central Antarctica, an unattended operating aerosol sampler was successfully deployed at the EPICA deep... -
Rare earth elements determined in Antarctic ice by inductively coupled plasma
Inductively coupled plasma mass spectrometry (ICP-MS) is a suitable tool for multi-element analysis at low concentration levels. Rare earth element (REE) determinations in... -
Aeolian dust and chemistry records from the EDML and EDC ice cores
To improve quantitative interpretation of ice core aeolian dust records a systematic methodical comparison has been made involving methods of water-insoluble particle counting... -
Lagrangian back-tracing results for Kohnen station given every 1 m of the depth
DEPTH in ice is modeled real depth; modeled ice equivalent depth at Kohnen: 2753.22 m; Modeled real depth at Kohnen including firn compaction: 2781.846 m; geographical... -
Lagrangian back-tracing results for Kohnen station given every 100 model years
Latitude and longitude are position of the place where Kohnen ice was deposited. Age is modeled, given in kiloyears before present.
