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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... -
Stable oxygen isotope profile of the B18_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... -
Depth-age model of the NGRIP_2012 firn core
Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the... -
Depth-age model of the B23_2012 firn core
Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the... -
Stable oxygen isotope profile of the B23_2012 firn core, annual means
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, annual means
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 B18_2012 firn core, annual means
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... -
Radiocarbon dates and calibrated ages of sediments enclosing ice wedges in th...
Radiocarbon dates and calibrated ages (99.7% probability) of sediments enclosing ice wedges in the northern part of Western Siberia and north-eastern part of the East European... -
δ¹⁸O, δ²H and deuterium excess values in the ice wedge ice and segregated ice...
δ¹⁸O, δ²H and deuterium excess (dexc) values in in the ice wedge ice (IW) and segregated ice (SI) lenses of the Yun'yaga peatland, Vorkuta region, and in the ice wedge ice from... -
δ¹⁸O, δ²H and deuterium excess values in snow from a snow patch in Vorkuta town
δ¹⁸O, δ²H and deuterium excess (dexc) values in snow from a snow patch in Vorkuta town (sampled December, 2018) and in the fresh snow (sampled December, 2005) during a single... -
Radiocarbon ages of the peat and wood remains of the Yun'yaga peatland, Vorku...
14C ages of bulk samples were obtained at the Institute of Geology RAS (lab code GIN) and in the Institute for the History of Material Culture, St. Petersburg (lab code Le).... -
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,... -
Calibrated 1.8 m stable water vapor isotope data from EastGRIP site on Greenl...
We present stable water isotope vapor measurements from the East GReenland Ice Sheet Project (EGRIP) location in the accumulation area of the Greenland Ice Sheet. The cavity... -
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... -
Snow stable water isotopes of a sublimation sampling scheme at the EastGRIP d...
Snow samples were taken along a 90 m transect at the EastGRIP ice core deep drilling site perpendicular to the prevailing wind direction.The snow was collected after... -
Snow stable water isotopes of a surface transect at the EastGRIP deep drillin...
Snow samples were taken on a daily basis along a 100 m wind-parallel transect at the EastGRIP ice core deep drilling site. The snow was collected in the morning at 11 positions... -
Snow stable water isotopes of a surface transect at the EastGRIP deep drillin...
Snow samples were taken on a daily basis along a 100 m wind-parallel transect at the EastGRIP ice core deep drilling site. The snow was collected in the morning at 11 positions... -
High-resolution stable water isotope and glacio-chemical composition of a fir...
The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The... -
Winter air temperature during the Holocene optimum in the north-eastern part ...
Early Holocene winter air temperatures have been reconstructed for the northeastern part of the East European Plain using stable isotope (δ18O and δ2H) records of syngenetic ice...
