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Chemistry versus age in firn core DML03C98_09
This dataset has no description
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Chemistry versus depth in firn core DML15C98_14
This dataset has no description
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Chemistry versus depth in firn core DML03C98_09
This dataset has no description
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Chemistry versus depth in firn core DML17C98_33 (B33)
This dataset has no description
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Chemistry versus age in firn core DML17C98_33 (B33)
This dataset has no description
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Geochemistry and physical properties of permafrost core L14-05
This dataset has no description
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Geochemistry and physical properties of permafrost core L14-04
This dataset has no description
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Geochemistry and physical properties of permafrost core L14-03
This dataset has no description
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Geochemistry and physical properties of permafrost core L14-02
This dataset has no description
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TemBi 2014 mesocosm study: Summer storm impact on water chemistry and physics...
We simulated an experimental summer storm in large-volume (~1200 m3, ~16m depth) enclosures in Lake Stechlin by mixing deeper water masses from the meta- and hypolimnion into... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Ground-ice stable isotope data from the pingo exposure AWI_12P-2208-A
Three profiles (12P-1908-A, 12P-2008-A, 12P-2208-A) of exposed ground ice were sampled in course of the expedition Pokhodsk 2012 in the Kolyma Lowland, which contained massive... -
Ground-ice stable isotope data from the pingo exposure AWI_12P-2008-A
Three profiles (12P-1908-A, 12P-2008-A, 12P-2208-A) of exposed ground ice were sampled in course of the expedition Pokhodsk 2012 in the Kolyma Lowland, which contained massive... -
Ground-ice stable isotope data from the pingo exposure AWI_12P-1908-A
Three profiles (12P-1908-A, 12P-2008-A, 12P-2208-A) of exposed ground ice were sampled in course of the expedition Pokhodsk 2012 in the Kolyma Lowland, which contained massive... -
Pore-water analyses of permafrost deposits from Byk_98_Mkh (Bykovsky Peninsul...
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 Byk_98_Mkh-6.2 (Bykovsky Peni...
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 Byk_98_Mkh-1.6.1 (Bykovsky Pe...
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...
