A combination of measurements from Autosub, an autonomous underwater vehicle, and ship-based instruments are used to describe the oceanographic conditions beneath Fimbul Ice Shelf, Antarctica. The data show an intricate oceanographic regime that is suggestive of variability at seasonal or longer time scales. Results from a numerical model of the flow beneath the ice shelf lend support to a strong seasonal variability, and data from instruments moored beneath the ice shelf show substantial temporal variations. The Autosub data indicate temperatures within the cavity somewhat lower than our model results would suggest; thus, our modeled melt rates (average of 0.85 m yr21) might be overestimates, although they are substantially lower than from...
The fate of the West Antarctic Ice Sheet is the largest remaining uncertainty in predicting sea-leve...
Fourteen phase-sensitive radars (ApRES) were deployed on the Filchner-Ronne Ice Shelf (FRIS) to meas...
Multiyear time series of ocean current and temperatures from beneath Filchner-Ronne Ice Shelf, Antar...
A combination of measurements from Autosub, an autonomous underwater vehicle, and ship-based instrum...
Antarctic ice shelves play a key role in the global climate system, acting as important sites for th...
The cavities beneath Antarctic ice shelves are among the least studied regions of the World Ocean, y...
Filchner-Ronne Ice Shelf (FRIS) is the world’s largest ice shelf by volume. It helps regulate Antarc...
Basal melting of ice shelves is inherently difficult to quantify through direct observations, yet it...
International audienceLimitations of access have long restricted exploration and investigation of th...
Limitations of access have long restricted exploration and investigation of the cavities beneath ice...
Melt water from the floating ice shelves at the margins of the southeastern Weddell Sea makes a sign...
Ocean circulation under ice shelves and associated rates of melting and freezing are strongly influ...
The interaction of ice shelves with the ocean water underneath is one of the key processes for the ...
Melt water from the floating ice shelves at the margins of the southeastern Weddell Sea makes a sign...
Limitations of access have long restricted exploration and investigation of the cavities beneath ice...
The fate of the West Antarctic Ice Sheet is the largest remaining uncertainty in predicting sea-leve...
Fourteen phase-sensitive radars (ApRES) were deployed on the Filchner-Ronne Ice Shelf (FRIS) to meas...
Multiyear time series of ocean current and temperatures from beneath Filchner-Ronne Ice Shelf, Antar...
A combination of measurements from Autosub, an autonomous underwater vehicle, and ship-based instrum...
Antarctic ice shelves play a key role in the global climate system, acting as important sites for th...
The cavities beneath Antarctic ice shelves are among the least studied regions of the World Ocean, y...
Filchner-Ronne Ice Shelf (FRIS) is the world’s largest ice shelf by volume. It helps regulate Antarc...
Basal melting of ice shelves is inherently difficult to quantify through direct observations, yet it...
International audienceLimitations of access have long restricted exploration and investigation of th...
Limitations of access have long restricted exploration and investigation of the cavities beneath ice...
Melt water from the floating ice shelves at the margins of the southeastern Weddell Sea makes a sign...
Ocean circulation under ice shelves and associated rates of melting and freezing are strongly influ...
The interaction of ice shelves with the ocean water underneath is one of the key processes for the ...
Melt water from the floating ice shelves at the margins of the southeastern Weddell Sea makes a sign...
Limitations of access have long restricted exploration and investigation of the cavities beneath ice...
The fate of the West Antarctic Ice Sheet is the largest remaining uncertainty in predicting sea-leve...
Fourteen phase-sensitive radars (ApRES) were deployed on the Filchner-Ronne Ice Shelf (FRIS) to meas...
Multiyear time series of ocean current and temperatures from beneath Filchner-Ronne Ice Shelf, Antar...