Principal Investigator: Tasha Snow (Earth System Science Interdisciplinary Center (ESSIC))

Co-Investigator(s): Susan Howard, Ellianna Abrahams, Matthew Siegfried

Collaborator(s): Laurie Padman, James Colliander


The overarching motivation of this project is to improve understanding of processes linking the ocean, sea ice (ice formed on the ocean), and glaciers along the Antarctic coast through a fusion of NASA Surface Water and Ocean Topography (SWOT), NASA Ice, Cloud, and land Elevation Satellite 2 (ICESat-2), and visible and thermal-infrared (heat) imagery datasets.

Through this work we will improve the SWOT mission’s broader sea surface and glacier height uncertainty quantification and open-source cloud-computing capabilities. Within this overarching motivation we have four specific goals:

  • Create time-varying sea surface and glacier height maps with verified and well-constrained geophysical corrections along the Antarctic coastline (e.g., tides, mean and dynamic ocean topography);
  • Evaluate SWOT glacier and sea surface height uncertainties in the presence of sea ice using ICESat-2 laser altimetry surface measurements;
  • Assess weather-band (few days) timescale fluctuations in near-ice-shelf circulation, ice, and ocean heat processes using a thermal and altimetry data fusion framework; and
  • Broaden SWOT collaborative open-science and cloud-computing frameworks.
Examples of HR data coverage, and validation of SWOT using ICESat-2 altimetry
Examples of HR data coverage, and validation of SWOT using ICESat-2 altimetry. (a) All SWOT HR tiles acquired over Larsen ice shelves, NW Weddell Sea, in Cycle 28 (14-24 February 2025) in the seasonal (austral summer) high-rate mask. Black contours show grounding line (point that ice transitions from grounded to floating), coastline, and the ice front from the MODIS Mosaic of Antarctica (MOA: Scambos et al., 2007; Haran et al., 2021), based on MODIS imagery from 2003-2004. Purple line shows recent ice front from Smith and Sutterley (2025). (b) Zoom of single HR tile (yellow rectangle in (a)) from 25 January 2025, showing map of WSE and three strong beams of a near-coincident ICESat-2 track (7.39 hr time separation). Yellow segments of each track are used in the histogram in (e). (c) Comparison of WSE (fully corrected) and hIS2 (fully corrected) along the central strong beam. (d) Difference between WSE and hIS2 for the same segment. (e) Histogram of (WSE-hIS2) for all three yellow-highlighted segments in (b).