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Ice properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
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... -
Ice surface measurements 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... -
Ice age uncertainty in ice cores 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 cores at core depth 1.95 m 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... -
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... -
Delta age in ice cores 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... -
Gas age uncertainty in ice cores 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... -
Radiocarbon AMS dating by organic microinclusions in the IW-17 sample from th...
The dating was carried out at the Laboratory of Radiocarbon Dating and Electron Microscopy, Institute of Geography (preparation of counted matter), and at the Center for Applied... -
Stable isotope (δ¹⁸O, δ²H and d) values, standard deviations, slopes and inte...
Stable isotope ratios (δ¹⁸O and δ²H) were analyzed at the stable isotope laboratory of the Faculty of Geography in the Lomonosov Moscow State University (headed by Prof. Yu.... -
Air temperature data from weather stations in Eastern Chukotka (for 1965–2015)
This dataset has no description
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High-resolution stable water isotope composition of firn cores OH-7, OH-11 an...
Firn cores OH-7 and OH-11 were retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula, at about 1130 m above sea level (a.s.l.).... -
Chronology, gas composition (CO2, CH4, N2O, δ18Oatm, δ15N-N2, δO2/N2, δAr/N2)...
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... -
δ¹⁸O values of Holocene and modern ice‐wedge ice on the Chukotka Peninsula an...
Stable oxygen isotopes composition (δ¹⁸O) in modern syngenetic ice wedges (recent ice veinlets - i.e. modern ice veins formed during the last 60-100 years and penetrated into... -
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 at 11 positions with 10 m... -
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 at 11 positions with 10 m... -
Snow stable water isotopes of a surface transect at the EastGRIP deep drillin...
Snow samples were taken on a daily basis along a 1000 m wind-parallel transect at the EastGRIP ice core deep drilling site. The snow was collected at 11 to 29 positions with 10... -
Snow stable water isotopes of a surface transect at the EastGRIP deep drillin...
Snow samples were taken on a daily basis along a 1000 m wind-parallel transect at the EastGRIP ice core deep drilling site. The snow was collected at 11 to 29 positions with 10... -
Snow Profiles of stable water isotopes at the EastGRIP deep drilling site, su...
Throughout the summer seasons 2016 to 2019 snow profiles were taken repeatedly. The sample positions are aligned along a 300 m wind-parallel transect at the EastGRIP ice core...
