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Airborne magnetic data across Riiser-Larsen Ice Shelf, East Antarctica, from ...
The airborne campaign 'RIISERBATHY' saw the acquisition of geophysical data across the Riiser-Larsen Ice Shelf in East Antarctica during the austral summer of 2022/2023, with... -
Bathymetric model beneath Riiser-Larsen Ice Shelf, East Antarctica, based on ...
Presented here is the first-ever bathymetric model beneath the Riiser-Larsen Ice Shelf, East Antarctica. The model is based on acquired airborne geophysical data across the ice... -
Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...
We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during... -
Snow density profiles from Neumayer station
This is a collection of shallow snow density data sets from research station Neumayer II, Neumayer III and the Kottas traverse between Neumayer, Kottas camp and Kohnen station.... -
Ice thickness radar data in Dronning Maud Land, East Antarctica, within GEA p...
Ice thickness radar data in Dronning Maud Land, East Antarctica, during the austral summer of 2015/2016 within the GEA project. GEA V (Geodynamic Evolutiuon of Antarctica) was... -
2005 to 2014 time series of Conductivity, Temperature, Depth (CTD) data from ...
Physical oceanography at the PerenniAL Acoustic Observatory in the Antarctic Ocean (Boebel et al. 2006). In the 2005/06 Antarctic field season, a Sea-Bird SBE37SM-RS232... -
Correspondence between AICC2023, AICC2012 and WD2014
This dataset has no description
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AICC2023, VOSTOK
This dataset has no description
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AICC2023, TALDICE
This dataset has no description
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AICC2023, NGRIP
This dataset has no description
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AICC2023, EDML
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AICC2023, EDC
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The Antarctic ice core chronology (AICC2023)
We present the new reference chronology (AICC2023) providing an age vs depth relationship covering the last 800 kyr (thousands of years) for five ice cores (EDC, EDML, NGRIP,... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Ground-penetrating radar data (50MHz) and internal reflection horizons along ...
The internal stratigraphic structure of ice shelves forms by the interplay of ice dynamics, snow accumulation and basal melt. To infer accumulation and basal melt rates, we... -
Ground-penetrating radar data (50MHz) and internal reflection horizons along ...
The internal stratigraphic structure of ice shelves forms by the interplay of ice dynamics, snow accumulation and basal melt. To infer accumulation and basal melt rates, we... -
Locations, outlines and ICESat-2 tracks of active lakes at the onset of the J...
We analysed a 6 year time series of displacement maps from Sentinel-1 SAR interferometry in the upstream region of Dronning Maud Lands Jutulstraumen Glacier (Antarctica). Our...
