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Illimani 2015 firn-core (Bolivia, 6300 m) black carbon record between 1995 to...
The glacier on Nevado Illimani in the eastern Bolivian Altiplano is one of the few in the mid- to low-latitudes giving access to ice covering the entire Holocene. The impurity... -
Extension of the stable oxygen isotope and density profile of the B26 ice 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 isotopologues of arrays of high resolution 1 m snow cores from a...
A set of 1 m firn profiles was sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station to quantify stratigraphic noise in high resolution isotope records. At... -
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... -
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. -
High-density crust record from firn core B40
This dataset has no description
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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...
