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A Simple Thermodynamic Model of the Internal Convective Zone of the Earth

As it is well known both atmospheric and mantle convection are very complex phenomena. The dynamical description of these processes is a very difficult task involving complicated 2-D or 3-D mathematical models. However, a first approximation to these phenomena can be by means of simplified thermodyn...

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Detalles Bibliográficos
Autores principales: Arango-Reyes, Karen, Barranco-Jiménez, Marco Antonio, Ares de Parga-Álvarez, Gonzalo, Angulo-Brown, Fernando
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7512586/
https://www.ncbi.nlm.nih.gov/pubmed/33266708
http://dx.doi.org/10.3390/e20120985