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High resolution δ¹⁸O, conductivity, and density of firn core DML641C02_01
This dataset has no description
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Low resolution conductivity and deuterium of ice core FRI12C92_15
Temperature of ice at 10 m depth: -23.8 deg C -
Conductivity and δ¹⁸O of ice core (saw dust) FRI12C92_15
Temperature of ice at 10 m depth: -23.8 deg C, measurements at saw dust samples -
High resolution density, conductivity, deuterium, and δ¹⁸O of ice core FRI12C...
Temperature of ice at 10 m depth: -23.8 deg C -
High resolution density, conductivity, deuterium, and δ¹⁸O of ice core FRI09C...
Temperature of ice at 10 m depth: -23.5 deg C -
GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and...
We present continuous records of 1 cm resolved sodium, sulfur, non-sea-salt sulfur, size-resolved insoluble particle concentrations and liquid conductivity using a Continuous... -
NGRIP ice-core volcanic sulfate concentration and deposition from 79.14 to 80...
We present continuous records of 1 cm resolved sulfate concentrations, insoluble particle number and mass concentration, and liquid conductivity using a Continuous Flow Analysis... -
Stable water isotope data from segregation ice of the Bol'shoy Lyakhovsky Isl...
Late Quaternary permafrost deposits on Big Lyakhovsky Island (New Siberian Islands, Russian Arctic) were studied with the aim of reconstructing the palaeoclimatic and... -
Pore-water analyses of permafrost deposits from Lya_1999_R8+50 Bol'shoy Lyakh...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_R22+60, Bol'shoy Lya...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_R18+50, Bol'shoy Lya...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_R17+30, Bol'shoy Lya...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_R17 , Bol'shoy Lyakh...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_R14+40, Bol'shoy Lya...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Lya_1999_L21+50, Bol'shoy Lya...
This dataset has no description
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Pore-water analyses of permafrost deposits from Lya_1999_2TZ, Bol'shoy Lyakho...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Stable water isotope data from seggregation ice of the Bykovsky Peninsula
This dataset has no description
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(Table 1) Dissolved organic carbon, water temperature and conductivity in thr...
Daphnia was collected from five subarctic ponds which differed greatly in their DOC contents and, consequently, their underwater light (UV) climates. Irrespective of which... -
Pore water geochemistry of sediment core BK-8
This dataset has no description
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Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, e...
Thermal permafrost degradation and coastal erosion in the Arctic remobilize substantial amounts of organic carbon (OC) and nutrients which have accumulated in late Pleistocene...
