Abstract
A glacier table consists of a rock supported by a slender column of ice and form naturally on glaciers. We investigate the onset of their formation at a smaller scale in a controlled environment. Depending on the size and thermal conductivity of a cap, it can either form of a table standing on an ice foot, or sink into the ice block. A one-dimension conduction model shows that the differential ice melting is controlled by a competition between two effects: a geometrical amplification, and a heat flux reduction due to the higher temperature of the cap as compared to the ice. Our model captures the transition between the two regimes and identifies a dimensionless number which controls the onset of glacier tables formation.
- Received 12 March 2021
- Accepted 29 July 2021
DOI:https://doi.org/10.1103/PhysRevLett.127.108501
© 2021 American Physical Society
Physics Subject Headings (PhySH)
Focus
How Glaciers Set a Table
Published 3 September 2021
Laboratory experiments reveal the melting process that generates a commonly seen ice feature called a glacier table.
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