Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces
During the late spring, most of the Arctic Ocean is covered by sea ice with a layer of snow on top. As the snow and sea ice begin to melt, water collects on the surface to form melt ponds. As melting progresses, sparse, disconnected ponds coalesce to form complex, self-similar structures which are c...
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ftdatacite:10.26053/0h-5ypy-ztg0 2023-05-15T14:58:33+02:00 Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces Bowen, Brady 2018 application/pdf https://dx.doi.org/10.26053/0h-5ypy-ztg0 https://collections.lib.utah.edu/ark:/87278/s6p59xdd en eng University of Utah Melt pond geometry article-journal Text ScholarlyArticle 2018 ftdatacite https://doi.org/10.26053/0h-5ypy-ztg0 2021-11-05T12:55:41Z During the late spring, most of the Arctic Ocean is covered by sea ice with a layer of snow on top. As the snow and sea ice begin to melt, water collects on the surface to form melt ponds. As melting progresses, sparse, disconnected ponds coalesce to form complex, self-similar structures which are connected over large length scales. The shapes undergo a transition in fractal dimension from 1 to about 2 around a critical length scale of 100 square meters, as found previously from area-perimeter data. Melt pond geometry depends strongly on sea ice and snow topography. Here we construct a rather simple model of melt pond boundaries as the intersection of a horizontal plane, representing the water level, with a random surface representing the topography. We show that an autoregressive class of anisotropic random Fourier surfaces provides topographies that yield the observed fractal dimension transition, with the ponds evolving and growing as the plane rises. The results are compared with a partial differential equation model of melt pond evolution that includes much of the physics of the system. Properties of the shift in fractal dimension, such as its amplitude, phase and rate, are shown to depend on the surface anisotropy and autocorrelation length scales in the models. Melting-driven differences between the two models are highlighted. Text Arctic Arctic Ocean Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean |
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DataCite Metadata Store (German National Library of Science and Technology) |
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language |
English |
topic |
Melt pond geometry |
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Melt pond geometry Bowen, Brady Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
topic_facet |
Melt pond geometry |
description |
During the late spring, most of the Arctic Ocean is covered by sea ice with a layer of snow on top. As the snow and sea ice begin to melt, water collects on the surface to form melt ponds. As melting progresses, sparse, disconnected ponds coalesce to form complex, self-similar structures which are connected over large length scales. The shapes undergo a transition in fractal dimension from 1 to about 2 around a critical length scale of 100 square meters, as found previously from area-perimeter data. Melt pond geometry depends strongly on sea ice and snow topography. Here we construct a rather simple model of melt pond boundaries as the intersection of a horizontal plane, representing the water level, with a random surface representing the topography. We show that an autoregressive class of anisotropic random Fourier surfaces provides topographies that yield the observed fractal dimension transition, with the ponds evolving and growing as the plane rises. The results are compared with a partial differential equation model of melt pond evolution that includes much of the physics of the system. Properties of the shift in fractal dimension, such as its amplitude, phase and rate, are shown to depend on the surface anisotropy and autocorrelation length scales in the models. Melting-driven differences between the two models are highlighted. |
format |
Text |
author |
Bowen, Brady |
author_facet |
Bowen, Brady |
author_sort |
Bowen, Brady |
title |
Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
title_short |
Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
title_full |
Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
title_fullStr |
Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
title_full_unstemmed |
Fractal geometry of melt ponds: Modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
title_sort |
fractal geometry of melt ponds: modeling the fractal geometry of arctic melt ponds using the level sets of random surfaces |
publisher |
University of Utah |
publishDate |
2018 |
url |
https://dx.doi.org/10.26053/0h-5ypy-ztg0 https://collections.lib.utah.edu/ark:/87278/s6p59xdd |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_doi |
https://doi.org/10.26053/0h-5ypy-ztg0 |
_version_ |
1766330688940802048 |