West Antarctica’s colossal glaciers are experiencing a rapid acceleration in melting, particularly since 2017. This alarming trend signals a decline in the ice shelf’s effectiveness in stabilizing the glacier.

Pine Island Glacier, the fastest-flowing glacier in Antarctica, significantly contributes to global sea level rise. This glacier plays a crucial role in the West Antarctic Ice Sheet, which has the potential to raise global sea levels by 5.3 meters if it fully melts.

The Pine Island Ice Shelf, extending into the ocean, is essential for holding back inland ice and shielding it from warm waters, potentially preventing 51 centimeters of sea level rise.

The instability of Pine Island Glacier, along with the nearby Thwaites Glacier, poses a significant risk to the longevity of the West Antarctic Ice Sheet.

Sarah Wells-Moran from the University of Chicago has been tracking the Pine Island Glacier using images from the Copernicus Sentinel 1 satellite, with data extending back to the 1970s.

The glacier’s velocity surged from 2.2 kilometers per year in 1974 to 4 kilometers per year by 2008 and reached nearly 5 kilometers per year from 2017 to 2023. This represents a 20 percent increase in just six years and a 113 percent increase since 1973.

Between 1973 and 2013, the ice flow from Pine Island Glacier accelerated by over 75%.

These changes have resulted in the glacier’s grounding line—the point at which the ice shelf begins to float—receding dramatically by more than 30 kilometers.

The researchers connected their findings to computer models, concluding that the ice shelf’s thinning and fractures allow warmer waters to penetrate further. This has led to the edge of the shelf “opening up,” as noted by Wells-Moran and her team.

They concluded that ice loss from West Antarctica is worsening due to the Pine Island ice shelf’s diminishing support for the upstream ice.

Sue Cook from the University of Tasmania stated that calving events alone cannot solely explain the acceleration of the glacier. She emphasized, “The damage to the glacier’s shear margin is likely the primary cause. This study corroborates that mechanism.”

Ted Scambos from the University of Colorado noted that warm ocean water is likely reaching the edge of the ice shelf in Pine Island Bay. “The loss of ice shelves may accelerate ocean circulation within the fjord, heightening circulation intensity where the glacier meets bedrock,” Scambos explained.

Nellie Abram from the Australian Antarctic Division remarked that this research will help determine the extent and rate at which the Pine Island ice shelf is collapsing. “It’s evident that the ice loss from this area will continue to affect coastlines worldwide for decades to come,” Abram stated.

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