‘Doomsday glacier’ that could trigger 6ft sea level rise is ‘holding on by its fingernails’

By | 07/09/2022

Antarctica’southward melting ‘Doomsday glacier’ could heighten body of water levels by 10 feet, scientists say

The loss of the Thwaites glacier could destabilize western Antarctica.

One of Antarctica’s most important glaciers is property on “by its fingernails” equally 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 amidst the fastest-changing glaciers in the region, according to scientists. Along with Pine Island, also located in the Amundsen Sea, the 2 structures are responsible for the largest contribution of ocean 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 h2o delivers heat to the present-day water ice-shelf crenel and melts its water ice shelves from below, according to a study published in Nature Geoscience on Mon.

Thwaites, which is about the size of Florida, has been known to exist on a fast retreat. Merely researchers from the University of South Florida’due south Higher of Marine Science and the British Antarctic Survey mapped a critical area of the seafloor in forepart of the glacier that could contribute to faster melting in the future.

PHOTO: Thwaites Glacier in West Antartica.



Thwaites Glacier in Due west Antartica.

James Youngel/NASA

Satellite imagery released in 2020 of Pino Island and Thwaites glaciers, which are located adjacent to each other, showed highly crevassed areas and open fractures — both signs that the shear zones on both glaciers, where the ice shelf is thin, had weakened structurally over the past decade.

But scientists have now discovered that the retreat from the grounding zone of Thwaites glacier is closer to more 2.1 kilometers per year — twice the rate observed by satellite imagery at the fastest-retreating part of the grounding between 2011 and 2019, according to the written report.

The researchers documented more than 160 parallel ridges that have been created as a result of the glacier’southward leading edge retreating and bobbing up and downwardly with the daily tides. In addition, the scientists analyzed the rib-similar formations submerged about a one-half of mile below the sea, determining that each new rib was likely formed over a single 24-hour interval.

Large calving events, when a large slice breaks off, occurred on Thwaites in October 2018 and Feb 2020, when an unprecedented retreat of the ice shelf occurred. The feedback process, likely triggered past new damage to the ice shelf, resulted in ice shelves being preconditioned for farther disintegration and large calving events.

PHOTO: An aerial view of Thwaites Glacier in West Antarctic, Jan. 30, 2019.



An aeriform view of Thwaites Glacier in W Antarctic, Jan. 30, 2019.

Jeremy Harbeck/OIB/NASA

This makes the ice shelves on Thwaites and Pine Isle more sensitive to extreme climate alter in the sea, temper and sea ice. If Thwaites and Pino Island were to destabilize, several of the neighboring areas would as well fall autonomously, causing a widespread collapse, the scientists said. Thwaites alone could cause sea levels to rise virtually 10 feet, the scientists said.

In December, researchers at the University of Colorado Boulder predicted that Thwaites will last only a few more years before information technology collapses.

“Thwaites is actually holding on today past its fingernails, and nosotros should wait to see big changes over small-scale timescales in the hereafter – even from one year to the next – in one case the glacier retreats beyond a shallow ridge in its bed,” said Robert Larter, a British Antarctic Survey marine geophysicist and a co-author of the study, in a statement.

Researchers from the U.Due south., the U.Thou. and Sweden used a state-of-the-fine art robotic vehicle loaded with imaging sensors, nicknamed “Ran,” to collect the imagery and supporting geophysical information, described past Anna Wahlin, a physical oceanographer from the University of Gothenburg, equally “a pioneering study of the ocean flooring.”

“The images Ran collected requite us vital insights into the processes happening at the disquisitional junction between the glacier and the ocean today,” Wahlin said.

Source: https://abcnews.go.com/International/antarcticas-melting-doomsday-glacier-raise-sea-levels-10/story?id=89415405