Ice shelf basal melt rates from a high-resolution digital elevation model (DEM) record for Pine Island Glacier, Antarctica

• Published in: The Cryosphere
• Main Authors: Shean, David E., Joughin, Ian R., Dutrieux, Pierre, Smith, Benjamin E., Berthier, Etienne
• Format: Text
• Language: English
• Published: 2019
• Subjects: Amundsen Sea; Pine Island Glacier; West Antarctica; Antarc*; Antarctica; Ice Shelf; Ice Shelves; Pine Island
• Online Access: https://doi.org/10.5194/tc-13-2633-2019; https://tc.copernicus.org/articles/13/2633/2019/

Ocean-induced basal melting is responsible for much of the Amundsen Sea Embayment ice loss in recent decades, but the total magnitude and spatiotemporal evolution of this melt is poorly constrained. To address this problem, we generated a record of high-resolution digital elevation models (DEMs) for Pine Island Glacier (PIG) using commercial sub-meter satellite stereo imagery and integrated additional 2002–2015 DEM and altimetry data. We implemented a Lagrangian elevation change (D h ∕ D t ) framework to estimate ice shelf basal melt rates at 32–256 m resolution. We describe this methodology and consider basal melt rates and elevation change over the PIG ice shelf and lower catchment from 2008 to 2015. We document the evolution of Eulerian elevation change (d h ∕ d t ) and upstream propagation of thinning signals following the end of rapid grounding line retreat around 2010. Mean full-shelf basal melt rates for the 2008–2015 period were ∼82 –93 Gt yr −1 , with ∼200 –250 m yr −1 basal melt rates within large channels near the grounding line, ∼10 –30 m yr −1 over the main shelf, and ∼0 –10 m yr −1 over the North shelf and South shelf, with the notable exception of a small area with rates of ∼50 –100 m yr −1 near the grounding line of a fast-flowing tributary on the South shelf. The observed basal melt rates show excellent agreement with, and provide context for, in situ basal melt-rate observations. We also document the relative melt rates for kilometer-scale basal channels and keels at different locations on the ice shelf and consider implications for ocean circulation and heat content. These methods and results offer new indirect observations of ice–ocean interaction and constraints on the processes driving sub-shelf melting beneath vulnerable ice shelves in West Antarctica.