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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... -
Monthly mean Lagrangian basal melt rates at Ekström Ice Shelf, Antarctica bet...
We estimated monthly mean basal melt rates in the Lagrangian frame from autonomous phase-sensitive radar (ApRES) measurements at the center of Ekström Ice Shelf, Antarctica... -
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... -
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... -
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...