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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/22282
Ver los metadatos del registro completo
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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 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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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 |
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eng |
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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 |
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Wiley |
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