Ising model for melt ponds on Arctic sea ice

Perhaps the most iconic feature of melting Arctic sea ice is the distinctive ponds that form on its surface. The geometrical patterns describing how melt water is distributed over the surface largely determine the solar reflectance and transmittance of the sea ice cover, which are key parameters in...

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Bibliographic Details
Published in:New Journal of Physics
Main Authors: Yi-Ping Ma, Ivan Sudakov, Courtenay Strong, Kenneth M Golden
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2019
Subjects:
Q
Online Access:https://doi.org/10.1088/1367-2630/ab26db
https://doaj.org/article/a35e34e39d574a6bba491b209e33c2d7
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spelling ftdoajarticles:oai:doaj.org/article:a35e34e39d574a6bba491b209e33c2d7 2023-09-05T13:16:45+02:00 Ising model for melt ponds on Arctic sea ice Yi-Ping Ma Ivan Sudakov Courtenay Strong Kenneth M Golden 2019-01-01T00:00:00Z https://doi.org/10.1088/1367-2630/ab26db https://doaj.org/article/a35e34e39d574a6bba491b209e33c2d7 EN eng IOP Publishing https://doi.org/10.1088/1367-2630/ab26db https://doaj.org/toc/1367-2630 doi:10.1088/1367-2630/ab26db 1367-2630 https://doaj.org/article/a35e34e39d574a6bba491b209e33c2d7 New Journal of Physics, Vol 21, Iss 6, p 063029 (2019) Arctic sea ice melt ponds Ising model metastable states fractal geometry Science Q Physics QC1-999 article 2019 ftdoajarticles https://doi.org/10.1088/1367-2630/ab26db 2023-08-13T00:38:44Z Perhaps the most iconic feature of melting Arctic sea ice is the distinctive ponds that form on its surface. The geometrical patterns describing how melt water is distributed over the surface largely determine the solar reflectance and transmittance of the sea ice cover, which are key parameters in climate modeling and upper ocean ecology. In order to help develop a predictive theoretical approach to studying melting sea ice, and the resulting patterns of light and dark regions on its surface in particular, we look to the statistical mechanics of phase transitions and introduce a two-dimensional random field Ising model which accounts for only the most basic physics in the system. The ponds are identified as metastable states in the model, where the binary spin variable corresponds to the presence of melt water or ice on the sea ice surface. With the lattice spacing determined by snow topography data as the only measured parameter input into the model, energy minimization drives the system toward realistic pond configurations from an initially random state. The model captures the essential mechanism of pattern formation of Arctic melt ponds, with predictions that agree very closely with observed scaling of pond sizes and transition in pond fractal dimension. Article in Journal/Newspaper Arctic Sea ice Directory of Open Access Journals: DOAJ Articles Arctic New Journal of Physics 21 6 063029
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic sea ice
melt ponds
Ising model
metastable states
fractal geometry
Science
Q
Physics
QC1-999
spellingShingle Arctic sea ice
melt ponds
Ising model
metastable states
fractal geometry
Science
Q
Physics
QC1-999
Yi-Ping Ma
Ivan Sudakov
Courtenay Strong
Kenneth M Golden
Ising model for melt ponds on Arctic sea ice
topic_facet Arctic sea ice
melt ponds
Ising model
metastable states
fractal geometry
Science
Q
Physics
QC1-999
description Perhaps the most iconic feature of melting Arctic sea ice is the distinctive ponds that form on its surface. The geometrical patterns describing how melt water is distributed over the surface largely determine the solar reflectance and transmittance of the sea ice cover, which are key parameters in climate modeling and upper ocean ecology. In order to help develop a predictive theoretical approach to studying melting sea ice, and the resulting patterns of light and dark regions on its surface in particular, we look to the statistical mechanics of phase transitions and introduce a two-dimensional random field Ising model which accounts for only the most basic physics in the system. The ponds are identified as metastable states in the model, where the binary spin variable corresponds to the presence of melt water or ice on the sea ice surface. With the lattice spacing determined by snow topography data as the only measured parameter input into the model, energy minimization drives the system toward realistic pond configurations from an initially random state. The model captures the essential mechanism of pattern formation of Arctic melt ponds, with predictions that agree very closely with observed scaling of pond sizes and transition in pond fractal dimension.
format Article in Journal/Newspaper
author Yi-Ping Ma
Ivan Sudakov
Courtenay Strong
Kenneth M Golden
author_facet Yi-Ping Ma
Ivan Sudakov
Courtenay Strong
Kenneth M Golden
author_sort Yi-Ping Ma
title Ising model for melt ponds on Arctic sea ice
title_short Ising model for melt ponds on Arctic sea ice
title_full Ising model for melt ponds on Arctic sea ice
title_fullStr Ising model for melt ponds on Arctic sea ice
title_full_unstemmed Ising model for melt ponds on Arctic sea ice
title_sort ising model for melt ponds on arctic sea ice
publisher IOP Publishing
publishDate 2019
url https://doi.org/10.1088/1367-2630/ab26db
https://doaj.org/article/a35e34e39d574a6bba491b209e33c2d7
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source New Journal of Physics, Vol 21, Iss 6, p 063029 (2019)
op_relation https://doi.org/10.1088/1367-2630/ab26db
https://doaj.org/toc/1367-2630
doi:10.1088/1367-2630/ab26db
1367-2630
https://doaj.org/article/a35e34e39d574a6bba491b209e33c2d7
op_doi https://doi.org/10.1088/1367-2630/ab26db
container_title New Journal of Physics
container_volume 21
container_issue 6
container_start_page 063029
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