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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... -
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01
The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the... -
Ultra-wideband radar data over the ice shelves and ice rises in eastern Dronn...
We present a high-resolution airborne radar data set (CHIRP 2019) for the Princess Ragnhild Coast, Dronning Maud Land, East Antarctica. The radar data has been acquired in... -
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... -
Basement topography and sediment thickness beneath Antarctica's Ross Ice Shel...
Depth to the magnetic basement beneath Antarctica's Ross Ice Shelf was determined from Werner deconvolution of ROSETTA-Ice airborne magnetic data. This process was constrained... -
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... -
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... -
UWBRAD 500-2000 MHz brightness temperature measurements during the ISSIUMAX c...
The dataset contains 500-2000 MHz brightness temperature measurements gathered by the Ultra-Wideband Software Defined Microwave Radiometer (UWBRAD) during the Ice Sheet and Sea... -
Sea floor depth under Ekström Ice Shelf, Antarctica, from seismic vibroseis s...
Sea floor depth under Ekström Ice Shelf, Antarctica - from seismic reflection profiles collected between 2010 and 2018. For each seismic profile, the reflection time of the sea... -
CTD profiles from beneath Ekstroem Ice Shelf and Atka Bay
CTD profiles of the water column beneath Ekstroem Ice Shelf and the adjacent Atka Bay. Ice shelf profiles were made through hot-water drilled access holes in the ice sheld and... -
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... -
Climate model response to increasing Antarctic iceberg and ice shelf melt
These data are outputs from climate simulations carried out using HadGEM3-GC3.1. The simulations are labelled ay187, az575, az576 and bb819, corresponding to experiments FW,... -
Sea floor bathymetry under Ekström Ice Shelf, Antarctica, from a compilation ...
A gridded bathymetry of the sea floor under Ekström Ice Shelf, Antarctica. The seismic data used to map the bathymetry were collected between 2010 and 2018, using two different... -
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...