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Locations of micro-inclusions identified with Raman spectroscopy in eleven sa...
Micro-inclusions in eleven samples from the upper 1340 m of the East Greenland Ice Core Project ice core in North-East Greenland were analysed with Raman spectroscopy. Ice... -
Grain size section mean data for the upper 1340 m of the EGRIP ice core and e...
Mean ice grain size and crystal-preferred orientation data was obtained from vertical thin sections (ca. 6.7 x 9 cm²) of the East Greenland Ice Core Project (EGRIP) ice core to... -
Microstructure maps with indicated micro-inclusions and grain boundaries (GB)...
High-resolution microstructure maps were created from several hundred micro-photographs from eleven samples from the upper 1340 m of the East Greenland Ice Core Project ice core... -
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... -
Ice Core Colle Gnifetti KCC
We analysed crystal-preferred orientation of c-axis and microstructure data from the Alpine ice core KCC at an unprecedented resolution and coverage of any Alpine ice core. We... -
Stable water isotopic concentration profile of the B26_2011 firn core
The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record... -
Depth-Age relationship of the B26_2011 firn core
The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record... -
Stable water isotopic concentration profile of the B26_2011 firn core, annual...
The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record... -
Accumulation rate of the B26_2011 firn core
The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record... -
Accumulation rate of the NG2012 firn core
The annual accumulation rate in water equivalent depth was derived based on the density measurements and the dating. -
Accumulation rate of the B23_2012 firn core
The annual accumulation rate in water equivalent depth was derived based on the density measurements and the dating. -
Accumulation rate of the B21_2012 firn core
The annual accumulation rate in water equivalent depth was derived based on the density measurements and the dating. -
Accumulation rate of the B18_2012 firn core
The annual accumulation rate in water equivalent depth was derived based on the density measurements and the dating. -
Density profile of the NG2012 firn core
Density was measured by micro-focus Computer Tomography with a resolution of 0.1mm and subsequently smoothed with a Gaussian filter with sigma 2 cm. -
Density profile of the B23_2012 firn core
Density was measured by micro-focus Computer Tomography with a resolution of 0.1mm and subsequently smoothed with a Gaussian filter with sigma 2 cm. -
Density profile of the B21_2012 firn core
Density was measured by micro-focus Computer Tomography with a resolution of 0.1mm and subsequently smoothed with a Gaussian filter with sigma 2 cm. -
Density profile of the B18_2012 firn core
Density was measured by micro-focus Computer Tomography with a resolution of 0.1mm and subsequently smoothed with a Gaussian filter with sigma 2 cm. -
Stable oxygen isotope profile of the NGRIP_2012 firn core
Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration... -
Stable oxygen isotope profile of the B23_2012 firn core
Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration... -
Stable oxygen isotope profile of the B21_2012 firn core
Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration...