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Barotropic modes, baroclinic modes and equivalent depths in the atmosphere

The equivalent depth of a rotating fluid layer determines the phase speed of all free (i.e. unforced) linear waves that propagate in it. The equivalent depth can be estimated from the eigenvalues of a second‐order differential equation for the vertical dynamics where the mean temperature profile is...

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Detalles Bibliográficos
Autores principales: De‐Leon, Yair, Paldor, Nathan, Garfinkel, Chaim I.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley & Sons, Ltd. 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7496845/
https://www.ncbi.nlm.nih.gov/pubmed/32981975
http://dx.doi.org/10.1002/qj.3781