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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... -
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... -
Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Rid...
Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore... -
Modeled bathymetry beneath Roi Baudouin and Borchgrevink ice shelves, East An...
The lack of consistent and reliable estimates of the bathymetry beneath the Roi Baudouin and Borchgrevink ice shelves of Dronning Maud Land is addressed by inverting airborne... -
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... -
Ice thickness, surface-, and bed elevation of a pinning point in Roi Baudouin...
This dataset describes ice thickness, surface elevation and bed elevation of a small pinning point located at the ice-shelf front of the Roi Baudouin Ice Shelf, Dronning Maud... -
Ice thickness, surface-, and bed elevation of Derwael Ice Rise, Dronning Maud...
This ASCII file contains ice thickness, surface- and bed elevation derived from radar surveys on Derwael Ice Rise in 2012 and 2013. Radar thickness/bed measurements use wave... -
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... -
Digitized ice edge form of the grounding zone of the Antarctic ice-sheet on 2...
Projection: EPSG:3031Ice edge form 31.12.2015Digitised in QGIS 3.10(64bit) from DLR satellite image:TDX1_SAR__EEC_RE___SC_S_SRA_20151231T003659_20151231T003728Rignot-et al.... -
Reverse ice flow calculations based on vector field ice flow data
Projection: EPSG:3031Reverse flow based on vector field ice flow data by: Rignot, E et al. (2017) -
Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Ridge
Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore... -
Smoothed alongtrack SMB estimates considered for krige estimation, which yiel...
This dataset has no description
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Corrected ICESat altimetry data for Antarctic ice shelves with links to shape...
These data are ICESat GLA12 428 spaceborne laser altimetry data . We have modified the original ICESat data by applying an improved tide model (CATS2008a) as well as the... -
Digitized ice edge form of the grounding zone of the Antarctic ice-sheet on 2...
Projection: EPSG:3031,Ice edge form 18.02.2018,Digitised in QGIS 3.10(64bit) from DLR satellite image:,TSX1_SAR__EEC_RE___SC_S_SRA_20180218T005416_20180218T005438