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Finite elements used in the vertical discretization of the fully compressible core of the ALADIN system
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| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.contributor.author | Vivoda, Jozef | es_ES |
| dc.contributor.author | Smolíková, Petra | es_ES |
| dc.contributor.author | Simarro Grande, Juan Pablo | es_ES |
| dc.date.accessioned | 2020-03-26T11:01:40Z | - |
| dc.date.available | 2020-03-26T11:01:40Z | - |
| dc.date.issued | 2018 | - |
| dc.identifier.citation | Monthly Weather Review. 2018, 146, p. 3293–3310 | es_ES |
| dc.identifier.issn | 0027-0644 | - |
| dc.identifier.issn | 1520-0493 | - |
| dc.identifier.uri | http://hdl.handle.net/20.500.11765/11529 | - |
| dc.description.abstract | The finite-element method with B splines is used for definition of vertical operators in the nonhydrostatic fully compressible dynamical core of the ALADIN system. It represents a generalization of the same method used in the hydrostatic dynamical core shared by the ALADIN system and the global forecast system ARPEGE/IFS. The method is shown to be robust enough in idealized academic tests and real simulations. Its theoretical superiority is shown when compared with the finite-difference method. | es_ES |
| dc.language.iso | eng | es_ES |
| dc.publisher | American Meteorological Society | es_ES |
| dc.subject | Dynamics | es_ES |
| dc.subject | Nonhydrostatic models | es_ES |
| dc.subject | Vertical coordinates | es_ES |
| dc.title | Finite elements used in the vertical discretization of the fully compressible core of the ALADIN system | es_ES |
| dc.type | info:eu-repo/semantics/article | es_ES |
| dc.relation.publisherversion | https://dx.doi.org/10.1175/MWR-D-18-0043.1 | es_ES |
| dc.rights.accessRights | info:eu-repo/semantics/openAccess | es_ES |
| Colecciones: | Artículos científicos 2015-2018 | |
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| Fichero | Descripción | Tamaño | Formato | ||
|---|---|---|---|---|---|
 | mwr-d-18-0043.1.pdf | 2,08 MB | Adobe PDF |  Visualizar/Abrir |
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