Registro completo de metadatos
| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.creator | Pulido, Manuel Arturo | - |
| dc.creator | Thuburn, John | - |
| dc.date | 2017-05-24T20:10:26Z | - |
| dc.date | 2017-05-24T20:10:26Z | - |
| dc.date | 2006-07 | - |
| dc.date | 2017-05-17T13:47:13Z | - |
| dc.date.accessioned | 2019-04-29T15:26:32Z | - |
| dc.date.available | 2019-04-29T15:26:32Z | - |
| dc.date.issued | 2006-07 | - |
| dc.identifier | Pulido, Manuel Arturo; Thuburn, John; Gravity wave drag estimation from global analyses using variational data assimilation principles. II: A case study.; Wiley; Quarterly Journal Of The Royal Meteorological Society; 132; 618; 7-2006; 1527-1543 | - |
| dc.identifier | 0035-9009 | - |
| dc.identifier | http://hdl.handle.net/11336/16931 | - |
| dc.identifier | 1477-870X | - |
| dc.identifier.uri | http://rodna.bn.gov.ar:8080/jspui/handle/bnmm/294237 | - |
| dc.description | An estimate of the three-dimensional gravity-wave drag field derived from middle-atmosphere analyses is presented. It is obtained using a novel technique based on variational data assimilation principles described in Part I. The assimilation is performed for a one-week period starting on 1 July 2002 using Met Office middle-atmosphere analyses as the observations as well as the initial condition. The rotational component of the gravity-wave drag is robustly estimated by the technique. The zonal-mean drag estimates reach maximum amplitudes of 50 m s−1day−1 at 0.4 hPa near the winter-hemisphere polar jet. In the middle stratosphere, drag estimates are much weaker with zonal-mean peak values of 5 m s−1day−1 and show transient small-scale features not obviously correlated with the local background flow. Vertical variations in the sign and pattern of the estimated drag suggest filtering of the gravity-wave spectrum by the background flow. | - |
| dc.description | 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 Tecnologica; Argentina. University Of Reading; Reino Unido | - |
| dc.description | Fil: Thuburn, John. University Of Reading; Reino Unido | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.language | eng | - |
| dc.publisher | Wiley | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1256/qj.05.43/abstract | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1256/qj.05.43 | - |
| dc.rights | info:eu-repo/semantics/restrictedAccess | - |
| dc.rights | https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ | - |
| dc.source | reponame:CONICET Digital (CONICET) | - |
| dc.source | instname:Consejo Nacional de Investigaciones Científicas y Técnicas | - |
| dc.source | instacron:CONICET | - |
| dc.subject | ADJOINT MODEL | - |
| dc.subject | MIDDLE ATMOSPHERE | - |
| dc.subject | PARAMETER ESTIMATION | - |
| dc.subject | TWIN EXPERIMENTS | - |
| dc.subject | Meteorología y Ciencias Atmosféricas | - |
| dc.subject | Ciencias de la Tierra y relacionadas con el Medio Ambiente | - |
| dc.subject | CIENCIAS NATURALES Y EXACTAS | - |
| dc.title | Gravity wave drag estimation from global analyses using variational data assimilation principles. II: A case study. | - |
| dc.type | info:eu-repo/semantics/article | - |
| dc.type | info:eu-repo/semantics/publishedVersion | - |
| dc.type | info:ar-repo/semantics/articulo | - |
| Aparece en las colecciones: | CONICET | |
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