Seismic, radio-echo, TWERLE balloon and oceanographic data of the Filchner-Ronne ice shelves are analysed. A large thin area in the central Ronne Ice Shelf is found to differ from the morphology of the Ross and Filchner ice shelves. This area is partly filled by basal saline ice, which can be attributed to regional regelation caused by oceanic circulation
For the Filchner-Ronne Ice Shelf we have compiled measurements of meteoric ice thickness from many i...
A two-dimensional plume model is used to study the interaction between Filchner-Ronne Ice Shelf, Ant...
Oceanographic data have been obtained from beneath the Ronne Ice Shelf at a site on the southeastern...
THE Filchner-Ronne ice shelf, which drains most of the marine-based portions of the West Antarctic i...
In an earlier study, melt/freeze rates beneath most of the Filchner–Ronne Ice Shelf, Antarctica, wer...
Detailed glaciological studies have been completed at 28 sites lying on an approximate flow line, ex...
The Filchner-Ronne ice shelf, which drains most of the marine-based portions of the West Antarctic i...
Aero-measurements during the 1983-84 and 1985-86 field seasons showed that the ice in the central pa...
Antarctica’s ice sheets don’t end at the coast, they extend onto the sea around the continent as ice...
Since 1981, the British Antarctic Survey has flown 27 000 line kilometres over Ronne Ice Shelf, duri...
Previous evidence suggests basal layer up to 400 m thick. Attempts to demonstrate that this consists...
The seabed morphology beneath the ice shelf is dominated by a slope down towards the interior of the...
Antarctic ice shelves play a key role in the global climate system, acting as important sites for th...
The Ninth Symposium on Polar Science/Special session: [S] Antarctic ice-ocean interaction ～observati...
We present oceanographic data from beneath the northern Ronne Ice Shelf. The data were collected dur...
For the Filchner-Ronne Ice Shelf we have compiled measurements of meteoric ice thickness from many i...
A two-dimensional plume model is used to study the interaction between Filchner-Ronne Ice Shelf, Ant...
Oceanographic data have been obtained from beneath the Ronne Ice Shelf at a site on the southeastern...
THE Filchner-Ronne ice shelf, which drains most of the marine-based portions of the West Antarctic i...
In an earlier study, melt/freeze rates beneath most of the Filchner–Ronne Ice Shelf, Antarctica, wer...
Detailed glaciological studies have been completed at 28 sites lying on an approximate flow line, ex...
The Filchner-Ronne ice shelf, which drains most of the marine-based portions of the West Antarctic i...
Aero-measurements during the 1983-84 and 1985-86 field seasons showed that the ice in the central pa...
Antarctica’s ice sheets don’t end at the coast, they extend onto the sea around the continent as ice...
Since 1981, the British Antarctic Survey has flown 27 000 line kilometres over Ronne Ice Shelf, duri...
Previous evidence suggests basal layer up to 400 m thick. Attempts to demonstrate that this consists...
The seabed morphology beneath the ice shelf is dominated by a slope down towards the interior of the...
Antarctic ice shelves play a key role in the global climate system, acting as important sites for th...
The Ninth Symposium on Polar Science/Special session: [S] Antarctic ice-ocean interaction ～observati...
We present oceanographic data from beneath the northern Ronne Ice Shelf. The data were collected dur...
For the Filchner-Ronne Ice Shelf we have compiled measurements of meteoric ice thickness from many i...
A two-dimensional plume model is used to study the interaction between Filchner-Ronne Ice Shelf, Ant...
Oceanographic data have been obtained from beneath the Ronne Ice Shelf at a site on the southeastern...
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