37 datasets found

Glacial ice can be dielectrically anisotropic due to ice fabric anisotropy, which describes a preferred orientation of ice crystal lattices, as well as structural anisotropy in...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 2008/09. The profiles extend across the eastern Dronning Maud Land ,...

This dataset contains airborne radar data acquired using the AWI EMR system (Nixdorf et al., 1999) during the Antarctic season of 2022/23. The airborne campaign 'RIISERBATHY'...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 2005/06. The profiles extend across the Dronning Maud Land over the...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 2001/02. The profiles extend across the western Dronning Maud Land...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 2000/01. The profiles extend across the western Dronning Maud Land...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 1998/99. The profiles extend across the western Dronning Maud Land on...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 1997/98. The profiles extend across the western Dronning Maud around...

This dataset contains airborne radar data acquired using the AWI EMR system during the Antarctic season of 1996/97. The profiles extend across the western Dronning Maud around...

Trajectory data for APEX floats 9223 and 9224 along Dronning Maud Land and Coats Land in the southern Weddell Sea from Mar 2022 - Feb 2023. The APEX floats were deployed during...

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...

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...

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...

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...

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...

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...

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...

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...

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...

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...