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Onset of Glacier Tables

Marceau Hénot, Nicolas Plihon, and Nicolas Taberlet
Phys. Rev. Lett. 127, 108501 – Published 3 September 2021
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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.

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  • 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)

Fluid DynamicsInterdisciplinary PhysicsPolymers & Soft MatterGeneral PhysicsNonlinear Dynamics

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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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Authors & Affiliations

Marceau Hénot, Nicolas Plihon, and Nicolas Taberlet*

  • Univ Lyon, ENS de Lyon, Univ Claude Bernard, CNRS, Laboratoire de Physique, F-69342 Lyon, France

  • *Corresponding author. nicolas.taberlet@ens-lyon.fr

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Issue

Vol. 127, Iss. 10 — 3 September 2021

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