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http://hdl.handle.net/20.500.11765/4859
A semi-implicit non-hydrostatic dynamical kernel using finite elements in the vertical discretization
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Campo DC | Valor | Lengua/Idioma |
---|---|---|
dc.contributor.author | Simarro Grande, Juan Pablo | es_ES |
dc.contributor.author | Hortal Reymundo, Mariano | es_ES |
dc.date.accessioned | 2016-11-10T10:37:55Z | - |
dc.date.available | 2016-11-10T10:37:55Z | - |
dc.date.issued | 2012 | - |
dc.identifier.citation | Quarterly Journal of the Royal Meteorological Society. 2012, 138(664), p. 826-839 | es_ES |
dc.identifier.issn | 0035-9009 | - |
dc.identifier.issn | 1477-870X | - |
dc.identifier.uri | http://hdl.handle.net/20.500.11765/4859 | - |
dc.description.abstract | This work is a first step in the direction of implementing a high-order finite-element discretization in the vertical in the non-hydrostatic version of the HARMONIE model. The present dynamical core of the HARMONIE model is shared with the ECMWF and the ALADIN models and uses a horizontal spectral discretization and a semi-implicit semi-Lagrangian time stepping scheme, all of which are maintained in this work. Trying to implement a finite-element discretization in the non-hydrostatic version of the HARMONIE model has been found to be very difficult due to the set of prognostic variables used and the mass-based vertical coordinate. A different set of prognostic variables and a hybrid vertical coordinate based on height are tested here on a vertical slice non-hydrostatic kernel. A stability analysis of the linear model has been done. To evaluate the model stability and accuracy, a set of test cases from the literature are presented in the linear and nonlinear regimes, with and without orography. An iterative centred-implicit scheme can be applied to avoid instability related to steep orography, although this reduces the efficiency of the model. The novel aspects with respect to existing non-hydrostatic model kernels are the use of cubic finite elements in the vertical discretization, the use of a height-based vertical coordinate in conjunction with a spectral discretization in the horizontal, and the coordinate-independent formulation of each element of the model including the semi-Lagrangian advection. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Wiley | es_ES |
dc.subject | Numerical weather prediction | es_ES |
dc.subject | Dynamical kernel | es_ES |
dc.subject | Non-hydrostatic | es_ES |
dc.subject | Vertical finite elements | es_ES |
dc.title | A semi-implicit non-hydrostatic dynamical kernel using finite elements in the vertical discretization | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.relation.publisherversion | https://dx.doi.org/10.1002/qj.952 | es_ES |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | es_ES |
Colecciones: | Artículos científicos 2010-2014 |
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Simarro_qrms_138.pdf | 549,99 kB | Adobe PDF | Visualizar/Abrir |
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