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100m-scale isotopic (δ18O) variability of the top-meter at location B52, East...
Small-scale (100 meter) isotopic composition of the top-meter of the snowpack around Kohnen station, Droning-Maud Land, East-Antarctica. The snow was sampled with the dual-tube... -
GEA IV 2013-15 radar ice thickness in eastern Dronning Maud Land
Ice thickness from radar data over eastern Dronning Maud Land, with geographical coordinates and dates of acquisition in 2013, 2014, and 2015. Airborne acquisition was completed... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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...