Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation

Autores
Pulido, Manuel Arturo; Thuburn, J.
Año de publicación
2005
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
A novel technique to estimate gravity wave drag from global-scale analyses is presented. It is based on the principles of four-dimensional variational data assimilation, using a dynamical model of the middle atmosphere and its adjoint. The global analyses are treated as observations. A cost function that measures the mismatch between the model state and observations is defined. The control variables are the components of the three-dimensional gravity wave drag field, so that minimization of the cost function gives the optimal gravity wave drag field. The minimization is performed using a conjugate gradient method, with the adjoint model used to calculate the gradient of the cost function. In this work, we present the theory behind the new technique and evaluate extensively the ability of the technique to estimate the gravity wave drag using so-called twin experiments, in which the ‘observations’ are given by the evolution of the dynamical model with a prescribed gravity wave drag. The results show that the technique can estimate accurately the prescribed gravity wave drag. When the cost function is suitably defined, there is good convergence of the minimization scheme under realistic atmospheric conditions. We also show that the cost function gradient is well approximated taking into account only adiabatic processes. We note some limitations of the technique for estimating gravity wave drag in tropical regions if satellite temperature measurements are the only observational information available.
Fil: Pulido, Manuel Arturo. University Of Reading; Reino Unido. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Thuburn, J.. University Of Reading; Reino Unido
Materia
Adjoint Model
Middle Atmosphere
Parameter Estimation
Twin Experiments
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:11336/22282

id CONICETDig_cf02f84b266d3e6ab207001f1a9e2f30
oai_identifier_str oai:ri.conicet.gov.ar:11336/22282
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementationPulido, Manuel ArturoThuburn, J.Adjoint ModelMiddle AtmosphereParameter EstimationTwin Experimentshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1A novel technique to estimate gravity wave drag from global-scale analyses is presented. It is based on the principles of four-dimensional variational data assimilation, using a dynamical model of the middle atmosphere and its adjoint. The global analyses are treated as observations. A cost function that measures the mismatch between the model state and observations is defined. The control variables are the components of the three-dimensional gravity wave drag field, so that minimization of the cost function gives the optimal gravity wave drag field. The minimization is performed using a conjugate gradient method, with the adjoint model used to calculate the gradient of the cost function. In this work, we present the theory behind the new technique and evaluate extensively the ability of the technique to estimate the gravity wave drag using so-called twin experiments, in which the ‘observations’ are given by the evolution of the dynamical model with a prescribed gravity wave drag. The results show that the technique can estimate accurately the prescribed gravity wave drag. When the cost function is suitably defined, there is good convergence of the minimization scheme under realistic atmospheric conditions. We also show that the cost function gradient is well approximated taking into account only adiabatic processes. We note some limitations of the technique for estimating gravity wave drag in tropical regions if satellite temperature measurements are the only observational information available.Fil: Pulido, Manuel Arturo. University Of Reading; Reino Unido. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Thuburn, J.. University Of Reading; Reino UnidoWiley2005-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/22282Pulido, Manuel Arturo; Thuburn, J.; Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation; Wiley; Quarterly Journal Of The Royal Meteorological Society; 131; 609; 7-2005; 1821-18400035-90091477-870XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1256/qj.04.116info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1256/qj.04.116/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:16:27Zoai:ri.conicet.gov.ar:11336/22282instacron: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:34982025-10-22 11:16:27.855CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
title Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
spellingShingle Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
Pulido, Manuel Arturo
Adjoint Model
Middle Atmosphere
Parameter Estimation
Twin Experiments
title_short Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
title_full Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
title_fullStr Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
title_full_unstemmed Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
title_sort Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation
dc.creator.none.fl_str_mv Pulido, Manuel Arturo
Thuburn, J.
author Pulido, Manuel Arturo
author_facet Pulido, Manuel Arturo
Thuburn, J.
author_role author
author2 Thuburn, J.
author2_role author
dc.subject.none.fl_str_mv Adjoint Model
Middle Atmosphere
Parameter Estimation
Twin Experiments
topic Adjoint Model
Middle Atmosphere
Parameter Estimation
Twin Experiments
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv A novel technique to estimate gravity wave drag from global-scale analyses is presented. It is based on the principles of four-dimensional variational data assimilation, using a dynamical model of the middle atmosphere and its adjoint. The global analyses are treated as observations. A cost function that measures the mismatch between the model state and observations is defined. The control variables are the components of the three-dimensional gravity wave drag field, so that minimization of the cost function gives the optimal gravity wave drag field. The minimization is performed using a conjugate gradient method, with the adjoint model used to calculate the gradient of the cost function. In this work, we present the theory behind the new technique and evaluate extensively the ability of the technique to estimate the gravity wave drag using so-called twin experiments, in which the ‘observations’ are given by the evolution of the dynamical model with a prescribed gravity wave drag. The results show that the technique can estimate accurately the prescribed gravity wave drag. When the cost function is suitably defined, there is good convergence of the minimization scheme under realistic atmospheric conditions. We also show that the cost function gradient is well approximated taking into account only adiabatic processes. We note some limitations of the technique for estimating gravity wave drag in tropical regions if satellite temperature measurements are the only observational information available.
Fil: Pulido, Manuel Arturo. University Of Reading; Reino Unido. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Thuburn, J.. University Of Reading; Reino Unido
description A novel technique to estimate gravity wave drag from global-scale analyses is presented. It is based on the principles of four-dimensional variational data assimilation, using a dynamical model of the middle atmosphere and its adjoint. The global analyses are treated as observations. A cost function that measures the mismatch between the model state and observations is defined. The control variables are the components of the three-dimensional gravity wave drag field, so that minimization of the cost function gives the optimal gravity wave drag field. The minimization is performed using a conjugate gradient method, with the adjoint model used to calculate the gradient of the cost function. In this work, we present the theory behind the new technique and evaluate extensively the ability of the technique to estimate the gravity wave drag using so-called twin experiments, in which the ‘observations’ are given by the evolution of the dynamical model with a prescribed gravity wave drag. The results show that the technique can estimate accurately the prescribed gravity wave drag. When the cost function is suitably defined, there is good convergence of the minimization scheme under realistic atmospheric conditions. We also show that the cost function gradient is well approximated taking into account only adiabatic processes. We note some limitations of the technique for estimating gravity wave drag in tropical regions if satellite temperature measurements are the only observational information available.
publishDate 2005
dc.date.none.fl_str_mv 2005-07
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/11336/22282
Pulido, Manuel Arturo; Thuburn, J.; Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation; Wiley; Quarterly Journal Of The Royal Meteorological Society; 131; 609; 7-2005; 1821-1840
0035-9009
1477-870X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/22282
identifier_str_mv Pulido, Manuel Arturo; Thuburn, J.; Gravity wave drag estimation from global analyses using variational data assimilation principles. I: Theory and implementation; Wiley; Quarterly Journal Of The Royal Meteorological Society; 131; 609; 7-2005; 1821-1840
0035-9009
1477-870X
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1256/qj.04.116
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1256/qj.04.116/abstract
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
dc.publisher.none.fl_str_mv Wiley
publisher.none.fl_str_mv Wiley
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
_version_ 1846781613840531456
score 12.982451