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Modelling 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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Detalles Bibliográficos
Autores principales: Gómez-Lozada, Felipe, del Valle, Carlos Andrés, Jiménez-Paz, Julián David, Lazarov, Boyan S., Galvis, Juan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10598449/
https://www.ncbi.nlm.nih.gov/pubmed/37885987
http://dx.doi.org/10.1098/rsos.230268