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...
Published in: | Physical Review Letters |
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Main Authors: | , , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Institute of Physics
2023
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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 |
id | ftunivromatorver:oai:art.torvergata.it:2108/362454 |
institution | Open Polar |
language | English |
op_collection_id | ftunivromatorver |
op_doi | https://doi.org/10.1103/PhysRevLett.131.234002 |
op_relation | 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 |
publishDate | 2023 |
publisher | American Institute of Physics |
record_format | openpolar |
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 |