Heterogeneous melting near the Thwaites Glacier grounding line.

ABSTRACT: Thwaites Glacier represents 15% of the ice discharge from the West Antarctic Ice Sheet and influences a wider catchment^1-3. Because it is grounded below sea level^4,5, Thwaites Glacier is thought to be susceptible to runaway retreat triggered at the grounding line (GL) at which the glacier reaches the ocean^6,7. Recent ice-flow acceleration^2,8 and retreat of the ice front^8-10 and GL^11,12 indicate that ice loss will continue. The relative impacts of mechanisms underlying recent retreat are however uncertain. Here we show sustained GL retreat from at least 2011 to 2020 and resolve mechanisms of ice-shelf melt at the submetre scale. Our conclusions are based on observations of the Thwaites Eastern Ice Shelf (TEIS) from an underwa

SUBMITTER: Schmidt BE 

PROVIDER: S-EPMC9931587 | biostudies-literature | 2023 Feb

REPOSITORIES: biostudies-literature