Articles | Volume 20, issue 11
https://doi.org/10.5194/tc-20-6263-2026
https://doi.org/10.5194/tc-20-6263-2026
Research article
 | 
03 Nov 2026
Research article |  | 03 Nov 2026

Seasonal icings reveal subsurface water drainage of a Greenland Ice Sheet outlet glacier

Rebecca McCerery, Joseph A. Graly, Christopher L. Hansen, Kate Winter, William P. Gilhooly III, Trinity L. Hamilton, Moses Jatta, Jeff R. Havig, Felipe Napoleoni, Alicia M. Rutledge, Matthew Terrell, Tanya M. Trott, Kayla Woodie, Bernd Kulessa, Sevi Modestou, Hannah Bahrani, Tori Kennedy, Alexandra Messerli, and Kathy Licht

Data sets

Geochemistry of proglacial waters from Isunnguata Sermia and Leverett Glacier, West Greenland, 2022-2024 (Version 1.0) Joseph A. Graly and Rebecca McCerery https://doi.org/10.5285/59406f3e-7971-4fe4-aa61-e1e112c84bce

Seasonal icings reveal subsurface water drainage of a Greenland Ice Sheet outlet glacier Rebecca McCerery and Joseph Graly https://doi.org/10.5281/zenodo.23159526

Download
Short summary
Ice cores from Isunnguata Sermia’s forefield reveal how proglacial naled and accreted ices form in Greenland. Naledi build up in winter from precipitation and mineral-rich subglacial water, while accreted ice forms in summer through supercooled water upwelling. Geophysical surveys indicate both are fed by subsurface flows potentially originating from the glacier bed. Here, we present the first conceptual model of these formations in Greenland.
Share
Altmetrics
Final-revised paper
Preprint