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Insoluble dust, ammonium, calcium, conductivity, peroxide and acid measured i...
Results from six firn cores obtained during a 426 km long northern Greenland traverse in 2015 between the NEEM and the EGRIP deep drilling stations situated on the Western and... -
Firn cores optained in Northern Greenlandin 2015
Results from six firn cores obtained during a 426 km long northern Greenland traverse in 2015 between the NEEM and the EGRIP deep drilling stations situated on the Western and... -
Nitrate chemistry of snow samples collected along the CHICTABA transect, East...
Nitrate samples were originally collected as 0.2-1.5 kg snow samples in the field along the CHICTABA traverse, Antarctica. Snow was collected in three methods: snow pits, skin... -
Snow temperature- and thermal conductivity data from a tundra and forest vege...
The data collection contains meteorological, soil and snow measurements from two nearby sites in the forest-tundra ecotone in the Tasiapik valley near Umiujaq in northern... -
Snow temperature- and thermal conductivity data from a second station at a tu...
The data collection contains meteorological, soil and snow measurements from two nearby sites in the forest-tundra ecotone in the Tasiapik valley near Umiujaq in northern... -
Summary of Bayesian onset detection algorithm for abrupt warming transitions ...
Summary statistics of posterior marginal distribution of the onset of abrupt warming transitions located in the last glacial age of the NGRIP record, based on both the d18O and... -
Gas properties in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Properties of ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Temperature and accumulation rate in ice cores from Larsen blue ice area, Eas...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CO2 in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
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... -
Snow stable water isotopes of a 0.5 cm deep sublimation sampling scheme at th...
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 1 cm deep sublimation sampling scheme at the ...
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 5 cm deep surface transect at the EastGRIP de...
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 0.5 cm deep surface transect at the EastGRIP ...
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 2 cm deep surface transect at the EastGRIP de...
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 1 cm deep surface transect at the EastGRIP de...
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 0.5 cm deep surface transect at the EastGRIP ...
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 2 cm deep surface transect at the EastGRIP de...
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...