Grounding Zone Dynamics
The study focuses on the "grounding zone," the area where ice transitions from resting on bedrock to floating on the ocean. Traditional models treated this boundary as a narrow, stable line. However, satellite radar data from the ICEYE constellation revealed that the grounding zone is several kilometres wide and shifts with the tides. This movement allows pressurized seawater to penetrate beneath the glacier’s grounded ice, lifting it and carrying ocean heat farther inland.
Eric Rignot, a professor of Earth system science at the University of California, Irvine, and co-author of the study, noted the significance of these findings. "We have documented and quantified the impacts of climate change on our planet’s sensitive ice sheets for decades, but a mounting realization gained in recent years of what is happening on the undersides of glaciers like Thwaites is leading to an even greater sense of alarm," Rignot said in a statement. "Our new model with more complete physics is able to match the record and then produces projections that are twice as large as before."