Antarctica's melting ‘Doomsday glacier’ could raise sea levels by 10 feet, scientists sayThe loss of the Thwaites glacier could destabilize western Antarctica.One of Antarctica's most important glaciers is holding on "by its fingernails" as warming temperatures around the globe threaten to cause further deterioration, which could then destabilize the glaciers in the entire region.
The Thwaites glacier, located in the Amundsen Sea in western Antarctica, is among the fastest-changing glaciers in the region, according to scientists. Along with Pine Island, also located in the Amundsen Sea, the two structures are responsible for the largest contribution of sea level rise out of Antarctica.Now, scientists are finding that the Thwaites glacier, also known as the “Doomsday glacier,” is melting faster than previously thought as warm and dense deep water delivers heat to the present-day ice-shelf cavity and melts its ice shelves from below, according to a study published in Nature Geoscience on Monday.
Thwaites, which is about the size of Florida, has been known to be on a fast retreat. But researchers from the University of South Florida's College of Marine Science and the British Antarctic Survey mapped a critical area of the seafloor in front of the glacier that could contribute to faster melting in the future.
a, Grounding at low water forms a rib by settling and sediment bulging/extrusion at the grounding line ahead of an ice plain. b, Subsequent grounding-line migration occurs during high water with the ice-shelf base displaced upwards and landwards by the tide, allowing contact with warm ocean water. Basal melting is enhanced by tidal mixing in the narrow cavity. c, Grounding line settles at new position on the next low water, creating a second rib in series. The amplitude and spacing of ribs is a function of tidal amplitude, which modulates the distance of retreat from ridge to ridge. Bottom: plot depicting typical diurnal tide cycle for a 48 h period at Thwaites Glacier. Intervals on x-axis correspond to 0.2 days (4.8 hours). a–c relate to positions on the tidal cycle. Triangles denote successive grounding-line positions. Note exaggerated vertical scale in all images; the true sea-floor expression of the ridges is subtle, with sea bed and ice bottom slopes only fractions of a degree.