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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-... -
(Supplement 3) EDML gas chronologies for the different scenarios 1 to 4
Scenario 1 is the same as scenario 3 for EDML (not shown here). Ice chronology is EDML1 (Ruth et al., Climate of the Past, 3, 475-484, http://www.clim-past.net/3/475/2007/;... -
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 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... -
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... -
EBSD analysis of subgrain boundaries and dislocation slip systems in Antarcti...
Ice has a very high plastic anisotropy with easy dislocation glide on basal planes while glide on non-basal planes is much harder. Basal glide involves dislocations with Burgers... -
Crystal c-axes (fabric G20) of ice core samples collected from the EDML ice c...
Device: AWI G20; spatial resolution: 525 µm/pix. See "Further details" for the field protocol. -
Crystal c-axes (fabric G50) of ice core samples collected from the EDML ice c...
See "Further details" for the field protocol. -
Eigenvalues of crystal orientation tensors for c-axes distributions of vertic...
This dataset has no description
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Eigenvalues of crystal orientation tensors for c-axes distributions of horizo...
This dataset has no description
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AICC2012 chronology for ice core EDML
This dataset has no description
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EPICA Dronning Maud Land carbon dioxide concentrations for the Last Millennium
This dataset has no description
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Stable isotopic methane (dD(CH4)) records of ice core EDML
All data are free of krypton interference during the mass spectrometric analysis. dD(CH4) data are measured using the system described in:Bock, M., J. Schmitt, J. Beck, R.... -
Rare earth elements determined in ice core EDML by laser-ablation inductively...
Only values exceeding the DL and the lowest concentrated standard are shown. -
X-ray microfocus computer tomography (MiXCT) from EDML ice core, from 150 to ...
See raw data at doi:10.1594/PANGAEA.782578 -
X-ray microfocus computer tomography (MiXCT) from EDML ice core, from 150 to ...
RAW files can be displayed with ImageJ (http://rsb.info.nih.gov/ij/). See the reconstruction at doi:10.1594/PANGAEA.782579 -
Raman signal of gaseous microinclusions in EDML ice
The file presents results from calculating the individual nitrogen, N2, to oxygen, O2, ratio of about 230 gaseous microinclusions (MIs) using the raw data of their respective...
