Preprints
https://doi.org/10.5194/egusphere-2026-1396
https://doi.org/10.5194/egusphere-2026-1396
20 Mar 2026
 | 20 Mar 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Temporal evolution of the Petermann Ice Shelf estuary constrained by remote sensing observations

Michela Savignano, Alison F. Banwell, Waleed Abdalati, Robin E. Bell, Alexandra Boghosian, W. Roger Buck, Sarah E. Esenther, Emily Glazer, Adam L. LeWinter, Laurence C. Smith, and Leigh A. Stearns

Abstract. Ice shelf rivers may reduce ice shelf instability by exporting surface meltwater from the ice shelf, limiting loading-induced stresses from ponded meltwater. However, if a supraglacial river incises to below sea level, forming an ice-shelf estuary, this mitigating effect may be negated. Water flow reversal in the estuary loads the ice shelf, inducing flexural stress, and prevents efficient meltwater export into the ocean. Evidence of this phenomenon has only been observed on the Petermann Ice Shelf in northern Greenland to date. A key factor in determining when and where ice-shelf estuaries form is river incision rate, defined as the decrease in channel bed elevation over time. Here we present a novel method for calculating incision rate in supraglacial rivers from paired multispectral WorldView-2/3 imagery and corresponding ArcticDEM strips. We apply this method over the Petermann Ice Shelf in 2014 and in 2016. The patterns of incision differ substantially between the two years, with the highest rates of incision occurring near the supraglacial river/estuary mouth in 2014, compared to the lowest incision rates at the same location in 2016. Using high-resolution satellite observations from WorldView imagery from 2013–2018 and modelled runoff, we conclude that the contrasting incision patterns are caused by the formation of the Petermann estuary and resultant water flow reversal, which inhibits efficient meltwater export. This in turn reduces frictional melting of the channel bottom and likely reduces the water surface slope, both of which cause the channel to cease deepening and become broader. Although the estuary appears to first form in August 2014, it is not present early in the 2016 melt season but does develop by early July. Similar observations made in subsequent melt seasons reveal a cyclical pattern whereby the estuary re-forms during each melt season as a result of meltwater and ocean water loading and unloading throughout the season.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Michela Savignano, Alison F. Banwell, Waleed Abdalati, Robin E. Bell, Alexandra Boghosian, W. Roger Buck, Sarah E. Esenther, Emily Glazer, Adam L. LeWinter, Laurence C. Smith, and Leigh A. Stearns

Status: open (until 01 May 2026)

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Michela Savignano, Alison F. Banwell, Waleed Abdalati, Robin E. Bell, Alexandra Boghosian, W. Roger Buck, Sarah E. Esenther, Emily Glazer, Adam L. LeWinter, Laurence C. Smith, and Leigh A. Stearns
Michela Savignano, Alison F. Banwell, Waleed Abdalati, Robin E. Bell, Alexandra Boghosian, W. Roger Buck, Sarah E. Esenther, Emily Glazer, Adam L. LeWinter, Laurence C. Smith, and Leigh A. Stearns
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Latest update: 20 Mar 2026
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Short summary
Supraglacial rivers carry meltwater across ice shelves, limiting ponding. However, if a river channel deepens below sea level, ocean water can flow back into it and form an ice-shelf estuary, trapping water on the ice shelf and increasing stresses that may weaken the ice. Using high-resolution satellite imagery and elevation data, we develop a new way to measure how quickly these rivers deepen, which we use to show that estuaries form seasonally, changing how meltwater drains from the ice shelf.
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