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High-resolution organic geochemical bulk parameter and biomarker records in s...
The Northeast Greenland continental shelf became one of the tipping elements in our climate system. Ongoing mass loss of the Greenland Ice Sheet, intensive sea-ice loss, the... -
Diatom assemblage of gravity core DG12-GC04 obtained on the Drygalski Basin i...
The samples for diatom assemblage were selected at nine horizons from GC01 and GC04, respectively. The sediment treatment, slide preparation, and diatom counting were carried... -
Diatom assemblage of gravity core DG12-GC01 obtained on the Drygalski Basin i...
The samples for diatom assemblage were selected at nine horizons from GC01 and GC04, respectively. The sediment treatment, slide preparation, and diatom counting were carried... -
Sediment properties of gravity core DG12-GC05 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC04 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC02 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC01 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Clay mineral composition of gravity core DG12-GC04 obtained on the Drygalski ...
The samples for clay mineral compositions were collected from GC01 and GC04 at 10 or 20 cm intervals. The organic matter was removed using 10% H2O2, and the fine fraction... -
Clay mineral composition of gravity core DG12-GC02 obtained on the Drygalski ...
The samples for clay mineral compositions were collected from GC01 and GC04 at 10 or 20 cm intervals. The organic matter was removed using 10% H2O2, and the fine fraction... -
Clay mineral composition of gravity core DG12-GC01 obtained on the Drygalski ...
The samples for clay mineral compositions were collected from GC01 and GC04 at 10 or 20 cm intervals. The organic matter was removed using 10% H2O2, and the fine fraction... -
Stable water isotopes (δ¹⁷O, δ¹⁸O, δD) from deep ice at Prudhoe Dome, NW Gree...
We present here a water isotope record (δ¹⁷O, δ¹⁸O, δD) from Prudhoe Dome, NW Greenland. The record spans the depth range 76.7–509.4 m (bedrock depth) and has a youngest age of... -
AWI EMR radar data upstream of the northern catchment of the Nioghalvfjerdsbr...
Here we present AWI EMR radio-echo sounding data in northeast Greenland upstream of the northern catchment of the Nioghalvfjerdsbrae (79°North Glacier; 79NG). The radar data... -
Sterols in sediment core PS100/270-1
This dataset has no description
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IP25 and highly branched isoprenoids in sediment core PS100/270-1
This dataset has no description
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Bulk parameters determined in sediment core PS100/270-1
This dataset has no description
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Streamlined subglacial bedforms across isolated topographic highs in the Puge...
These data include shapefiles of streamlined subglacial bedforms, elongate bedforms created at the glacier-bed interface by erosional and depositional processes, characterized... -
Streamlined subglacial bedforms across the deglaciated Northern Hemisphere
These data include shapefiles of streamlined subglacial bedforms, elongate bedforms created at the glacier-bed interface by erosional and depositional processes, characterized... -
Drainage basin delineation for outlet glaciers of Northeast Greenland based o...
The drainage divides of ice sheets separate the overall glaciated area into multiple sectors. These drainage basins are essential for partitioning mass changes of the ice sheet,... -
Supraglacial river discharge into Moulin L41A on the Greenland Ice Sheet meas...
Supraglacial river discharge was measured by monitoring water depth with a custom-built pressure sensor, at 1-minute intervals, and converting depth to discharge with a rating... -
Proglacial river discharge from the Greenland Ice Sheet measured in spring/su...
Proglacial river discharge was monitored using stage measurements (collected by a HOBO pressure sensor) and dye dilution gauging at a stable bedrock section near the terminus of...
