fegomezl/Brinicle: Modeling and simulation of brinicle formation ...

Below the Arctic sea ice, under the right conditions, a flux of icy brine flows down into the sea. The icy brine has a much lower fusion point and is denser than normal seawater. As a result, it sinks while freezing everything around it, forming an ice channel called a brinicle (also known as ice st...

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Main Authors: Gómez-Lozada, Felipe, del Valle, Carlos Andrés, Jímenez-Paz, Julian David, Lazarov, Boyan S., Galvis, Juan
Format: Software
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.8384885
https://zenodo.org/record/8384885
id ftdatacite:10.5281/zenodo.8384885
record_format openpolar
spelling ftdatacite:10.5281/zenodo.8384885 2023-11-05T03:39:39+01:00 fegomezl/Brinicle: Modeling and simulation of brinicle formation ... Gómez-Lozada, Felipe del Valle, Carlos Andrés Jímenez-Paz, Julian David Lazarov, Boyan S. Galvis, Juan 2023 https://dx.doi.org/10.5281/zenodo.8384885 https://zenodo.org/record/8384885 en eng Zenodo https://github.com/fegomezl/Brinicle/tree/article https://github.com/fegomezl/Brinicle/tree/article https://dx.doi.org/10.5281/zenodo.8384884 Open Access info:eu-repo/semantics/openAccess Finite element method Nonlinear dynamics Multiphysics Phase change Ocean dynamics Chemical Garden Software article SoftwareSourceCode 2023 ftdatacite https://doi.org/10.5281/zenodo.838488510.5281/zenodo.8384884 2023-10-09T11:08:24Z Below the Arctic sea ice, under the right conditions, a flux of icy brine flows down into the sea. The icy brine has a much lower fusion point and is denser than normal seawater. As a result, it sinks while freezing everything around it, forming an ice channel called a brinicle (also known as ice stalactite). In this paper, we develop a mathematical model for this phenomenon, assuming cylindrical symmetry. The fluid is considered to be viscous and quasi-stationary. The heat and salt transport are weakly coupled to the fluid motion and are modeled with the corresponding conservation equations, accounting for diffusive and convective effects. Finite element discretization is employed to solve the coupled system of partial differential equations. We find that the model can capture the general behavior of the physical system and generate brinicle-like structures while also recovering dendrite composition, which is a physically expected feature aligned with previous experimental results. This represents the first ... Software Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Finite element method
Nonlinear dynamics
Multiphysics
Phase change
Ocean dynamics
Chemical Garden
spellingShingle Finite element method
Nonlinear dynamics
Multiphysics
Phase change
Ocean dynamics
Chemical Garden
Gómez-Lozada, Felipe
del Valle, Carlos Andrés
Jímenez-Paz, Julian David
Lazarov, Boyan S.
Galvis, Juan
fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
topic_facet Finite element method
Nonlinear dynamics
Multiphysics
Phase change
Ocean dynamics
Chemical Garden
description Below the Arctic sea ice, under the right conditions, a flux of icy brine flows down into the sea. The icy brine has a much lower fusion point and is denser than normal seawater. As a result, it sinks while freezing everything around it, forming an ice channel called a brinicle (also known as ice stalactite). In this paper, we develop a mathematical model for this phenomenon, assuming cylindrical symmetry. The fluid is considered to be viscous and quasi-stationary. The heat and salt transport are weakly coupled to the fluid motion and are modeled with the corresponding conservation equations, accounting for diffusive and convective effects. Finite element discretization is employed to solve the coupled system of partial differential equations. We find that the model can capture the general behavior of the physical system and generate brinicle-like structures while also recovering dendrite composition, which is a physically expected feature aligned with previous experimental results. This represents the first ...
format Software
author Gómez-Lozada, Felipe
del Valle, Carlos Andrés
Jímenez-Paz, Julian David
Lazarov, Boyan S.
Galvis, Juan
author_facet Gómez-Lozada, Felipe
del Valle, Carlos Andrés
Jímenez-Paz, Julian David
Lazarov, Boyan S.
Galvis, Juan
author_sort Gómez-Lozada, Felipe
title fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
title_short fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
title_full fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
title_fullStr fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
title_full_unstemmed fegomezl/Brinicle: Modeling and simulation of brinicle formation ...
title_sort fegomezl/brinicle: modeling and simulation of brinicle formation ...
publisher Zenodo
publishDate 2023
url https://dx.doi.org/10.5281/zenodo.8384885
https://zenodo.org/record/8384885
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation https://github.com/fegomezl/Brinicle/tree/article
https://github.com/fegomezl/Brinicle/tree/article
https://dx.doi.org/10.5281/zenodo.8384884
op_rights Open Access
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.838488510.5281/zenodo.8384884
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