Beneath the floating Filchner-Ronne Ice Shelf in West Antarctica, scientists have discovered huge ice channels that are 800 feet high and stretch for hundreds of miles. The discovery, by researchers from the University of Exeter, Newcastle University, the University of Bristol, the University of Edinburgh, the British Antarctic Survey, and the University of York is detailed in the journal Nature Geoscience.
The channels were discovered by British researchers using satellite images and airborne radar measurements. The channels can also be seen on the surface of the ice shelf, as the ice floats at a different height depending on its thickness.
The researchers also predicted the path of meltwater flowing under the part of the ice in contact with the land (known as the ice sheet). They discovered that the predicted flow paths lined up with the channels under the ice shelf at the point where the ice starts to float.
The match-up indicates that the water flow beneath the grounded ice sheet is responsible for the formation of the channels beneath the floating ice shelf. When the meltwater flowing under the ice sheet enters the ocean beneath the ice shelf, it causes a plume of ocean water to form, which then melts out the vast channels under the ice shelf.
Channels of this magnitude have been observed before elsewhere, but their formation has been attributed to purely oceanic processes rather than meltwater exiting the grounded ice sheet.
“If we are to understand the behaviour of the ice sheet, and its contribution to changes in sea level, we need to fully understand the role of water at the base of the ice sheet. The information gained from these newly discovered channels will enable us to understand more fully how the water system works and, hence, how the ice sheet will behave in the future,” said researcher Anne Le Brocq, from the University of Exeter
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