A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation

Autores
Pulido, Manuel Arturo; Rodas, Claudio José Francisco
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Ray techniques are a promising tool for developing orographic gravity wave drag schemes. However, the modeling of the propagation of orographic waves using standard ray theory in realistic background wind conditions usually encounters several regions, called caustics, where the first-order ray approximation breaks down. In this work the authors develop a higher-order approximation than standard ray theory, named the Gaussian beam approximation, for orographic gravity waves in a background wind that depends on height. The analytical results show that this formulation is free of the singularities that arise in ray theory. Orographic gravity waves that propagate in a background wind that turns with height?the same conditions as in the work of Shutts?are examined under the Gaussian beam approximation. The evolution of the amplitude is well defined in this approximation even at caustics and at the forcing level. When comparing results from the Gaussian beam approximation with high-resolution numerical simulations that compute the exact solution, there is good agreement of the amplitude and phase fields. Realistic orography is represented by means of a superposition of multiple Gaussians in wavenumber space that fit the spectrum of the orography. The technique appears to give a good representation of the disturbances generated by flow over realistic orography.
Fil: Pulido, Manuel Arturo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Instituto de Modelado e Innovación Tecnológica. Universidad Nacional del Nordeste. Facultad de Ciencias Exactas Naturales y Agrimensura. Instituto de Modelado e Innovación Tecnológica; Argentina
Fil: Rodas, Claudio José Francisco. Universidad Nacional del Nordeste; Argentina
Materia
GRAVITY WAVES
NUMERICAL ANALYSIS/MODELING
OROGRAPHIC EFFECTS
WIND
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/148687

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spelling A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximationPulido, Manuel ArturoRodas, Claudio José FranciscoGRAVITY WAVESNUMERICAL ANALYSIS/MODELINGOROGRAPHIC EFFECTSWINDhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1Ray techniques are a promising tool for developing orographic gravity wave drag schemes. However, the modeling of the propagation of orographic waves using standard ray theory in realistic background wind conditions usually encounters several regions, called caustics, where the first-order ray approximation breaks down. In this work the authors develop a higher-order approximation than standard ray theory, named the Gaussian beam approximation, for orographic gravity waves in a background wind that depends on height. The analytical results show that this formulation is free of the singularities that arise in ray theory. Orographic gravity waves that propagate in a background wind that turns with height?the same conditions as in the work of Shutts?are examined under the Gaussian beam approximation. The evolution of the amplitude is well defined in this approximation even at caustics and at the forcing level. When comparing results from the Gaussian beam approximation with high-resolution numerical simulations that compute the exact solution, there is good agreement of the amplitude and phase fields. Realistic orography is represented by means of a superposition of multiple Gaussians in wavenumber space that fit the spectrum of the orography. The technique appears to give a good representation of the disturbances generated by flow over realistic orography.Fil: Pulido, Manuel Arturo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Instituto de Modelado e Innovación Tecnológica. Universidad Nacional del Nordeste. Facultad de Ciencias Exactas Naturales y Agrimensura. Instituto de Modelado e Innovación Tecnológica; ArgentinaFil: Rodas, Claudio José Francisco. Universidad Nacional del Nordeste; ArgentinaAmer Meteorological Soc2011-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/148687Pulido, Manuel Arturo; Rodas, Claudio José Francisco; A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 68; 1; 1-2011; 46-600022-4928CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/atsc/68/1/2010jas3468.1.xmlinfo:eu-repo/semantics/altIdentifier/doi/10.1175/2010JAS3468.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:51:13Zoai:ri.conicet.gov.ar:11336/148687instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:51:13.356CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
title A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
spellingShingle A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
Pulido, Manuel Arturo
GRAVITY WAVES
NUMERICAL ANALYSIS/MODELING
OROGRAPHIC EFFECTS
WIND
title_short A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
title_full A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
title_fullStr A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
title_full_unstemmed A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
title_sort A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation
dc.creator.none.fl_str_mv Pulido, Manuel Arturo
Rodas, Claudio José Francisco
author Pulido, Manuel Arturo
author_facet Pulido, Manuel Arturo
Rodas, Claudio José Francisco
author_role author
author2 Rodas, Claudio José Francisco
author2_role author
dc.subject.none.fl_str_mv GRAVITY WAVES
NUMERICAL ANALYSIS/MODELING
OROGRAPHIC EFFECTS
WIND
topic GRAVITY WAVES
NUMERICAL ANALYSIS/MODELING
OROGRAPHIC EFFECTS
WIND
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Ray techniques are a promising tool for developing orographic gravity wave drag schemes. However, the modeling of the propagation of orographic waves using standard ray theory in realistic background wind conditions usually encounters several regions, called caustics, where the first-order ray approximation breaks down. In this work the authors develop a higher-order approximation than standard ray theory, named the Gaussian beam approximation, for orographic gravity waves in a background wind that depends on height. The analytical results show that this formulation is free of the singularities that arise in ray theory. Orographic gravity waves that propagate in a background wind that turns with height?the same conditions as in the work of Shutts?are examined under the Gaussian beam approximation. The evolution of the amplitude is well defined in this approximation even at caustics and at the forcing level. When comparing results from the Gaussian beam approximation with high-resolution numerical simulations that compute the exact solution, there is good agreement of the amplitude and phase fields. Realistic orography is represented by means of a superposition of multiple Gaussians in wavenumber space that fit the spectrum of the orography. The technique appears to give a good representation of the disturbances generated by flow over realistic orography.
Fil: Pulido, Manuel Arturo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Nordeste. Instituto de Modelado e Innovación Tecnológica. Universidad Nacional del Nordeste. Facultad de Ciencias Exactas Naturales y Agrimensura. Instituto de Modelado e Innovación Tecnológica; Argentina
Fil: Rodas, Claudio José Francisco. Universidad Nacional del Nordeste; Argentina
description Ray techniques are a promising tool for developing orographic gravity wave drag schemes. However, the modeling of the propagation of orographic waves using standard ray theory in realistic background wind conditions usually encounters several regions, called caustics, where the first-order ray approximation breaks down. In this work the authors develop a higher-order approximation than standard ray theory, named the Gaussian beam approximation, for orographic gravity waves in a background wind that depends on height. The analytical results show that this formulation is free of the singularities that arise in ray theory. Orographic gravity waves that propagate in a background wind that turns with height?the same conditions as in the work of Shutts?are examined under the Gaussian beam approximation. The evolution of the amplitude is well defined in this approximation even at caustics and at the forcing level. When comparing results from the Gaussian beam approximation with high-resolution numerical simulations that compute the exact solution, there is good agreement of the amplitude and phase fields. Realistic orography is represented by means of a superposition of multiple Gaussians in wavenumber space that fit the spectrum of the orography. The technique appears to give a good representation of the disturbances generated by flow over realistic orography.
publishDate 2011
dc.date.none.fl_str_mv 2011-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/148687
Pulido, Manuel Arturo; Rodas, Claudio José Francisco; A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 68; 1; 1-2011; 46-60
0022-4928
CONICET Digital
CONICET
url http://hdl.handle.net/11336/148687
identifier_str_mv Pulido, Manuel Arturo; Rodas, Claudio José Francisco; A higher-order ray approximation applied to orographic gravity waves: Gaussian beam approximation; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 68; 1; 1-2011; 46-60
0022-4928
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/atsc/68/1/2010jas3468.1.xml
info:eu-repo/semantics/altIdentifier/doi/10.1175/2010JAS3468.1
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Amer Meteorological Soc
publisher.none.fl_str_mv Amer Meteorological Soc
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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