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Bathymetry beneath ice shelves of western Dronning Maud Land, East Antarctica
The lack of consistent and reliable estimates of the bathymetry beneath the ice shelves of western Dronning Maud Land is addressed by inverting airborne gravity data to model... -
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
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AICC2023, EDML
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AICC2023, EDC
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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... -
Airborne radio-echo sounding data from Jutulstraumen Glacier (western Dronnin...
Radio-echo sounding (RES) data from Jutulstraumen Glacier in western Dronning Maud Land (East Antarctica) recorded with the Alfred Wegener Institutes multi-channel... -
Local snow dunes / sastrugi heights across the plateau of Dronning Maud Land,...
Local snow surface heights were sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station. They were used to quantify surface roughness and its relation to... -
Stable water isotopologues of arrays of high resolution 1 m snow cores from a...
A set of 1 m firn profiles was sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station to quantify stratigraphic noise in high resolution isotope records. At... -
Ice thickness from the coast of Dronning Maud Land (Antarctica), recorded 201...
Ice thickness from the coast of Dronning Maud Land (Antarctica), recorded 2018/19 with the AWI UWB radar systemThis project aims to acquire airborne data with AWI's UWB... -
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... -
Ultra-wideband radar profiles over the Roi Baudouin Ice Shelf in Dronning Mau...
The Roi Baudouin Ice Shelf is located in an ice-shelf belt surrounding coastal Dronning Maud Land, East Antarctica. Here, we provide two radar profiles on the ice shelf, which...