A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach

In this paper, the equation for the gravity wave spectra in mean atmosphere is analytically solved without linearization by the Adomian decomposition method. As a consequence, the nonlinear nature of problem is preserved and the errors found in the results are only due to the parameterization. The r...

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Main Authors: Antonio Gledson Goulart, Davidson Martins Moreira, Luiz Cláudio Pimentel, Jesus Salvador Pérez Guerrero
Format: Article
Language:English
Published: Sociedade Brasileira de Meteorologia 2013-12-01
Series:Revista Brasileira de Meteorologia
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862013000400001&lng=en&tlng=en
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spelling doaj-456aa1c98f0a4ee09879756694d7edf62020-11-24T20:50:39ZengSociedade Brasileira de MeteorologiaRevista Brasileira de Meteorologia1982-43512013-12-0128435736310.1590/S0102-77862013000400001S0102-77862013000400001A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approachAntonio Gledson Goulart0Davidson Martins Moreira1Luiz Cláudio Pimentel2Jesus Salvador Pérez Guerrero3Universidade Federal do PampaUniversidade Federal da Fronteira SulUniversidade Federal do Rio de JaneiroComissão Nacional de Energia NuclearIn this paper, the equation for the gravity wave spectra in mean atmosphere is analytically solved without linearization by the Adomian decomposition method. As a consequence, the nonlinear nature of problem is preserved and the errors found in the results are only due to the parameterization. The results, with the parameterization applied in the simulations, indicate that the linear solution of the equation is a good approximation only for heights shorter than ten kilometers, because the linearization the equation leads to a solution that does not correctly describe the kinetic energy spectra.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862013000400001&lng=en&tlng=enespectro de ondas de gravidademédia atmosferamétodo da decomposição
collection DOAJ
language English
format Article
sources DOAJ
author Antonio Gledson Goulart
Davidson Martins Moreira
Luiz Cláudio Pimentel
Jesus Salvador Pérez Guerrero
spellingShingle Antonio Gledson Goulart
Davidson Martins Moreira
Luiz Cláudio Pimentel
Jesus Salvador Pérez Guerrero
A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
Revista Brasileira de Meteorologia
espectro de ondas de gravidade
média atmosfera
método da decomposição
author_facet Antonio Gledson Goulart
Davidson Martins Moreira
Luiz Cláudio Pimentel
Jesus Salvador Pérez Guerrero
author_sort Antonio Gledson Goulart
title A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
title_short A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
title_full A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
title_fullStr A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
title_full_unstemmed A solution of nonlinear equation for the gravity wave spectra from Adomian decomposition method: a first approach
title_sort solution of nonlinear equation for the gravity wave spectra from adomian decomposition method: a first approach
publisher Sociedade Brasileira de Meteorologia
series Revista Brasileira de Meteorologia
issn 1982-4351
publishDate 2013-12-01
description In this paper, the equation for the gravity wave spectra in mean atmosphere is analytically solved without linearization by the Adomian decomposition method. As a consequence, the nonlinear nature of problem is preserved and the errors found in the results are only due to the parameterization. The results, with the parameterization applied in the simulations, indicate that the linear solution of the equation is a good approximation only for heights shorter than ten kilometers, because the linearization the equation leads to a solution that does not correctly describe the kinetic energy spectra.
topic espectro de ondas de gravidade
média atmosfera
método da decomposição
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862013000400001&lng=en&tlng=en
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