The corresponding increased ice sheet mass loss has often followed thinning, reduction or loss of ice shelves or loss of
floating glacier tongues.
Not exact matches
Along the coastline, the
floating tongues of
glaciers are breaking up.
Its
floating front edge, the Totten ice shelf, sticks out like a
tongue over the water and acts as a buttress for the giant
glacier, slowing its movement toward the ocean.
Scientists previously thought that only
glaciers with sturdy, cold ice, such as in Greenland, could form
floating tongues.
Ice shelves are
floating tongues of ice that extend from grounded
glaciers on land.
Once again the key to this
glacier's second major ice loss this decade after limited retreat in the last century, is thinning of the
floating tongue, which weakens the
glacier.
In the Amundsen Sea Embayment region of West Antarctica, where
glaciers terminate in the ocean and extend over the waters via
floating ice
tongues, six major
glaciers are experiencing rapid rates of retreat.
The recent increases in outlet
glacier discharge have always been coincident with
floating tongue losses.
In 1997, the
floating tongue of Jakobshavn
Glacier, the largest outlet of the Greenland Ice Sheet, began to disintegrate, and simultaneously the dynamic thinning of the
glacier began.
Instead, the
glacier develops a
floating ice
tongue - a shelf of ice that extends from the main body of the
glacier out onto the waters of the fjord.
Upon reaching the sea, a number of these large outlet
glaciers extend into the water with a
floating «ice
tongue».