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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. -
Bulk and position-specific isotopic composition of N2O (total and in situ) an...
The mixing ratio and bulk isotopic composition of nitrous oxide (N2O) was measured after wet extraction and purification of the air enclosed in 150 g ice core samples from EDC,... -
EDML ice-core volcanic sulfate concentration and deposition from 78.97 to 79....
We present continuous records of ca. 2 cm resolved sulfate concentrations using a Continuous Flow Analysis (CFA) system (Röthlisberger et al., 2000; Severi et al., 2007; Wegner... -
Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
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... -
Stable water isotopes (δ18O) of ice core EDML from 2416 m to 2773.5 m
The European Project for Ice Coring in Antarctica (EPICA) focused on the drilling of two deep ice cores, the first at Dome C (EDC) and the second at Kohnen station (75°00' S,... -
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... -
Reconstructed volcanic stratospheric sulfur injections and volcanic sulfate d...
We used four polar ice cores - two from Greenland and two from Antarctica - to investigate volcanic sulphate deposition on polar ice sheets between 13,200 and 12,800 years BP.... -
Density of firn core B52
We present density information of firn core B52. B52 was drilled in the Antarctic summer season 2012/13 in January 2013 as part of the ANT-Land_2012_COFI campagin. The cores... -
Stable oxygen isotopes of ice core EDML
Version 2 - 2010-11-26 - replaces the dataset see other version- remeasurements, lost and found samples or means of hiRes measurements; in a few cases linear interpolated-... -
Thick-section images of the EPICA-Dronning-Maud-Land (EDML) ice core
This data set consists of 3.5 Million images with a total size of 313 GByte. -
Antarctic δ18Oice and atmospheric temperature stacks of the WD, EDC, and EDML...
This dataset consists in two stacks of three Antarctic records (EDC, EDML, and WD), one for δ18Oice and the other for atmospheric temperature: both stacks are provided with... -
High-density crust record from snow samples ANT-Land_2016_COFI, East Antarctica
This dataset has no description
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High-density crust record from snow samples ANT-Land_2016_COFI_27a, East Anta...
This dataset has no description
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Stable water isotopes and major ions in snow along a traverse route between K...
At the majority of the sampling locations, 4 snow profiles in a triangle setup (one profile in the center surrounded by the others with 10m spacing) have been sampled. The... -
Stable water isotopes and major ions in snow along a traverse route between K...
At the majority of the sampling locations, 4 snow profiles in a triangle setup (one profile in the center surrounded by the others with 10m spacing) have been sampled. The... -
Stable water isotopes and major ions in snow along a traverse route between K...
At the majority of the sampling locations, 4 snow profiles in a triangle setup (one profile in the center surrounded by the others with 10m spacing) have been sampled. The...
