Tangent method for the arctic curve arising from freezing boundaries

In the paper [1], the authors study the arctic curve arising in random tilings of some planar domains with an arbitrary distribution of defects on one edge. Using the tangent method they derive a parametric equation for portions of arctic curve in terms of an arbitrary piecewise differentiable funct...

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Main Authors: Debin, Bryan, Ruelle, Philippe
Other Authors: UCL - SST/IRMP - Institut de recherche en mathématique et physique
Format: Report
Language:English
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/2078.1/212642
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spelling ftunistlouisbrus:oai:dial.uclouvain.be:boreal:212642 2023-05-15T14:35:10+02:00 Tangent method for the arctic curve arising from freezing boundaries Debin, Bryan Ruelle, Philippe UCL - SST/IRMP - Institut de recherche en mathématique et physique 2018 http://hdl.handle.net/2078.1/212642 eng eng boreal:212642 http://hdl.handle.net/2078.1/212642 info:eu-repo/semantics/workingPaper 2018 ftunistlouisbrus 2019-07-03T22:17:34Z In the paper [1], the authors study the arctic curve arising in random tilings of some planar domains with an arbitrary distribution of defects on one edge. Using the tangent method they derive a parametric equation for portions of arctic curve in terms of an arbitrary piecewise differentiable function that describes the defect distribution. When this distribution presents "freezing" intervals, other portions of arctic curve appear and typically have a cusp. These freezing boundaries can be of two types, respectively with maximal or minimal density of defects. Our purpose here is to extend the tangent method derivation of [1] to include these portions, hence providing the proof of the conjectures made in [1]. Report Arctic DIAL@USL-B (Université Saint-Louis, Bruxelles) Arctic
institution Open Polar
collection DIAL@USL-B (Université Saint-Louis, Bruxelles)
op_collection_id ftunistlouisbrus
language English
description In the paper [1], the authors study the arctic curve arising in random tilings of some planar domains with an arbitrary distribution of defects on one edge. Using the tangent method they derive a parametric equation for portions of arctic curve in terms of an arbitrary piecewise differentiable function that describes the defect distribution. When this distribution presents "freezing" intervals, other portions of arctic curve appear and typically have a cusp. These freezing boundaries can be of two types, respectively with maximal or minimal density of defects. Our purpose here is to extend the tangent method derivation of [1] to include these portions, hence providing the proof of the conjectures made in [1].
author2 UCL - SST/IRMP - Institut de recherche en mathématique et physique
format Report
author Debin, Bryan
Ruelle, Philippe
spellingShingle Debin, Bryan
Ruelle, Philippe
Tangent method for the arctic curve arising from freezing boundaries
author_facet Debin, Bryan
Ruelle, Philippe
author_sort Debin, Bryan
title Tangent method for the arctic curve arising from freezing boundaries
title_short Tangent method for the arctic curve arising from freezing boundaries
title_full Tangent method for the arctic curve arising from freezing boundaries
title_fullStr Tangent method for the arctic curve arising from freezing boundaries
title_full_unstemmed Tangent method for the arctic curve arising from freezing boundaries
title_sort tangent method for the arctic curve arising from freezing boundaries
publishDate 2018
url http://hdl.handle.net/2078.1/212642
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation boreal:212642
http://hdl.handle.net/2078.1/212642
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