Bistability in Radiatively Heated Melt Ponds

Melting and solidification processes, intertwined with convective flows, play a fundamental role in geophysical contexts. One of these processes is the formation of melt ponds on glaciers, ice shelves, and sea ice. It is driven by solar radiation and is of great significance for Earth's heat ba...

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Published in:Physical Review Letters
Main Authors: Rui Yang, Christopher J. Howland, Hao-Ran Liu, Roberto Verzicco, Detlef Lohse
Other Authors: Yang, R, Howland, Cj, Liu, H, Verzicco, R, Lohse, D
Format: Article in Journal/Newspaper
Language:English
Published: American Institute of Physics 2023
Subjects:
Online Access:https://hdl.handle.net/2108/362454
https://doi.org/10.1103/PhysRevLett.131.234002
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author Rui Yang
Christopher J. Howland
Hao-Ran Liu
Roberto Verzicco
Detlef Lohse
author2 Yang, R
Howland, Cj
Liu, H
Verzicco, R
Lohse, D
author_facet Rui Yang
Christopher J. Howland
Hao-Ran Liu
Roberto Verzicco
Detlef Lohse
author_sort Rui Yang
collection Universitá degli Studi di Roma "Tor Vergata": ART - Archivio Istituzionale della Ricerca
container_issue 23
container_title Physical Review Letters
container_volume 131
description Melting and solidification processes, intertwined with convective flows, play a fundamental role in geophysical contexts. One of these processes is the formation of melt ponds on glaciers, ice shelves, and sea ice. It is driven by solar radiation and is of great significance for Earth's heat balance, as it significantly lowers the albedo. Through direct numerical simulations and theoretical analysis, we unveil a bistability phenomenon in the melt pond dynamics. As solar radiation intensity and the melt pond's initial depth vary, an abrupt transition occurs: this tipping point transforms the system from a stable fully frozen state to another stable equilibrium state, characterized by a distinct melt pond depth. The physics of this transition can be understood within a heat flux balance model, which exhibits excellent agreement with our numerical results. Together with the Grossmann-Lohse theory for internally heated convection, the model correctly predicts the bulk temperature and the flow strength within the melt ponds, offering insight into the coupling of phase transitions with adjacent turbulent flows and the interplay between convective melting and radiation-driven processes.
format Article in Journal/Newspaper
genre Ice Shelves
Sea ice
genre_facet Ice Shelves
Sea ice
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spelling ftunivromatorver:oai:art.torvergata.it:2108/362454 2025-05-11T14:21:11+00:00 Bistability in Radiatively Heated Melt Ponds Rui Yang Christopher J. Howland Hao-Ran Liu Roberto Verzicco Detlef Lohse Yang, R Howland, Cj Liu, H Verzicco, R Lohse, D 2023 https://hdl.handle.net/2108/362454 https://doi.org/10.1103/PhysRevLett.131.234002 eng eng American Institute of Physics country:US info:eu-repo/semantics/altIdentifier/wos/WOS:001153352800005 volume:131 issue:23 journal:PHYSICAL REVIEW LETTERS https://hdl.handle.net/2108/362454 doi:10.1103/PhysRevLett.131.234002 Settore ING-IND/06 info:eu-repo/semantics/article 2023 ftunivromatorver https://doi.org/10.1103/PhysRevLett.131.234002 2025-04-15T04:42:29Z Melting and solidification processes, intertwined with convective flows, play a fundamental role in geophysical contexts. One of these processes is the formation of melt ponds on glaciers, ice shelves, and sea ice. It is driven by solar radiation and is of great significance for Earth's heat balance, as it significantly lowers the albedo. Through direct numerical simulations and theoretical analysis, we unveil a bistability phenomenon in the melt pond dynamics. As solar radiation intensity and the melt pond's initial depth vary, an abrupt transition occurs: this tipping point transforms the system from a stable fully frozen state to another stable equilibrium state, characterized by a distinct melt pond depth. The physics of this transition can be understood within a heat flux balance model, which exhibits excellent agreement with our numerical results. Together with the Grossmann-Lohse theory for internally heated convection, the model correctly predicts the bulk temperature and the flow strength within the melt ponds, offering insight into the coupling of phase transitions with adjacent turbulent flows and the interplay between convective melting and radiation-driven processes. Article in Journal/Newspaper Ice Shelves Sea ice Universitá degli Studi di Roma "Tor Vergata": ART - Archivio Istituzionale della Ricerca Physical Review Letters 131 23
spellingShingle Settore ING-IND/06
Rui Yang
Christopher J. Howland
Hao-Ran Liu
Roberto Verzicco
Detlef Lohse
Bistability in Radiatively Heated Melt Ponds
title Bistability in Radiatively Heated Melt Ponds
title_full Bistability in Radiatively Heated Melt Ponds
title_fullStr Bistability in Radiatively Heated Melt Ponds
title_full_unstemmed Bistability in Radiatively Heated Melt Ponds
title_short Bistability in Radiatively Heated Melt Ponds
title_sort bistability in radiatively heated melt ponds
topic Settore ING-IND/06
topic_facet Settore ING-IND/06
url https://hdl.handle.net/2108/362454
https://doi.org/10.1103/PhysRevLett.131.234002