Gravity wave activity in the mesopause region from airglow measurements at El Leoncito
- Autores
- Reisin, Esteban Rodolfo; Scheer, Jurgen
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Based on almost 1000 nights of OH(6-2) and O2b(0-1) airglow data measured during 1998–2002 at El Leoncito (31:8◦S, 69:2◦W), seasonal variations of gravity wave activity are determined from temperature and intensity variances. The photon-counting technique used permits to derive the individual statistical errors a priori, and to quantitatively isolate the geophysical variance. The two airglow emissions yield results for the altitudes of 87 and 95 km. Tidal activity contains most of the variance (especially between March and October) and therefore must be suppressed to obtain gravity wave activity. There are strong night-to-night variations, from completely quiet to variances of more than 80 K2 in temperature. The interannual variability was small enough to de;ne a meaningful seasonal climatology. The wave activity variation is semiannual, similar to previous radar wind results, including those at the same latitude, and has its main maximum in southern winter and a weaker maximum in summer. The growth of wave activity from 87 to 95 km, when interpreted in terms of an amplitude growth factor, leads to a value of 1:35 ± 0:01, similar to the one obtained for tides, in a previous paper of ours. From the comparison of intensity and temperature variance for a given emission, mean values of Krassovsky’s are derived (5:60 ± 0:09 for OH, and 5:08 ± 0:08 for O2), that compare favourably with results obtained from individual wave signatures. This proves the consistency between the wave activities derived from intensities and temperatures.
Fil: Reisin, Esteban Rodolfo. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina
Fil: Scheer, Jurgen. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina - Materia
- Gravity
- 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:11336/22201
Ver los metadatos del registro completo
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Gravity wave activity in the mesopause region from airglow measurements at El LeoncitoReisin, Esteban RodolfoScheer, JurgenGravityhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1Based on almost 1000 nights of OH(6-2) and O2b(0-1) airglow data measured during 1998–2002 at El Leoncito (31:8◦S, 69:2◦W), seasonal variations of gravity wave activity are determined from temperature and intensity variances. The photon-counting technique used permits to derive the individual statistical errors a priori, and to quantitatively isolate the geophysical variance. The two airglow emissions yield results for the altitudes of 87 and 95 km. Tidal activity contains most of the variance (especially between March and October) and therefore must be suppressed to obtain gravity wave activity. There are strong night-to-night variations, from completely quiet to variances of more than 80 K2 in temperature. The interannual variability was small enough to de;ne a meaningful seasonal climatology. The wave activity variation is semiannual, similar to previous radar wind results, including those at the same latitude, and has its main maximum in southern winter and a weaker maximum in summer. The growth of wave activity from 87 to 95 km, when interpreted in terms of an amplitude growth factor, leads to a value of 1:35 ± 0:01, similar to the one obtained for tides, in a previous paper of ours. From the comparison of intensity and temperature variance for a given emission, mean values of Krassovsky’s are derived (5:60 ± 0:09 for OH, and 5:08 ± 0:08 for O2), that compare favourably with results obtained from individual wave signatures. This proves the consistency between the wave activities derived from intensities and temperatures.Fil: Reisin, Esteban Rodolfo. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; ArgentinaFil: Scheer, Jurgen. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; ArgentinaElsevier2004-12info: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/11336/22201Reisin, Esteban Rodolfo; Scheer, Jurgen; Gravity wave activity in the mesopause region from airglow measurements at El Leoncito; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 66; 6-9; 12-2004; 655-6611364-6826CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S136468260400029Xinfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jastp.2004.01.017info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T12:06:12Zoai:ri.conicet.gov.ar:11336/22201instacron: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 12:06:12.654CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| title |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| spellingShingle |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito Reisin, Esteban Rodolfo Gravity |
| title_short |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| title_full |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| title_fullStr |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| title_full_unstemmed |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| title_sort |
Gravity wave activity in the mesopause region from airglow measurements at El Leoncito |
| dc.creator.none.fl_str_mv |
Reisin, Esteban Rodolfo Scheer, Jurgen |
| author |
Reisin, Esteban Rodolfo |
| author_facet |
Reisin, Esteban Rodolfo Scheer, Jurgen |
| author_role |
author |
| author2 |
Scheer, Jurgen |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
Gravity |
| topic |
Gravity |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.3 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Based on almost 1000 nights of OH(6-2) and O2b(0-1) airglow data measured during 1998–2002 at El Leoncito (31:8◦S, 69:2◦W), seasonal variations of gravity wave activity are determined from temperature and intensity variances. The photon-counting technique used permits to derive the individual statistical errors a priori, and to quantitatively isolate the geophysical variance. The two airglow emissions yield results for the altitudes of 87 and 95 km. Tidal activity contains most of the variance (especially between March and October) and therefore must be suppressed to obtain gravity wave activity. There are strong night-to-night variations, from completely quiet to variances of more than 80 K2 in temperature. The interannual variability was small enough to de;ne a meaningful seasonal climatology. The wave activity variation is semiannual, similar to previous radar wind results, including those at the same latitude, and has its main maximum in southern winter and a weaker maximum in summer. The growth of wave activity from 87 to 95 km, when interpreted in terms of an amplitude growth factor, leads to a value of 1:35 ± 0:01, similar to the one obtained for tides, in a previous paper of ours. From the comparison of intensity and temperature variance for a given emission, mean values of Krassovsky’s are derived (5:60 ± 0:09 for OH, and 5:08 ± 0:08 for O2), that compare favourably with results obtained from individual wave signatures. This proves the consistency between the wave activities derived from intensities and temperatures. Fil: Reisin, Esteban Rodolfo. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina Fil: Scheer, Jurgen. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina |
| description |
Based on almost 1000 nights of OH(6-2) and O2b(0-1) airglow data measured during 1998–2002 at El Leoncito (31:8◦S, 69:2◦W), seasonal variations of gravity wave activity are determined from temperature and intensity variances. The photon-counting technique used permits to derive the individual statistical errors a priori, and to quantitatively isolate the geophysical variance. The two airglow emissions yield results for the altitudes of 87 and 95 km. Tidal activity contains most of the variance (especially between March and October) and therefore must be suppressed to obtain gravity wave activity. There are strong night-to-night variations, from completely quiet to variances of more than 80 K2 in temperature. The interannual variability was small enough to de;ne a meaningful seasonal climatology. The wave activity variation is semiannual, similar to previous radar wind results, including those at the same latitude, and has its main maximum in southern winter and a weaker maximum in summer. The growth of wave activity from 87 to 95 km, when interpreted in terms of an amplitude growth factor, leads to a value of 1:35 ± 0:01, similar to the one obtained for tides, in a previous paper of ours. From the comparison of intensity and temperature variance for a given emission, mean values of Krassovsky’s are derived (5:60 ± 0:09 for OH, and 5:08 ± 0:08 for O2), that compare favourably with results obtained from individual wave signatures. This proves the consistency between the wave activities derived from intensities and temperatures. |
| publishDate |
2004 |
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2004-12 |
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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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http://hdl.handle.net/11336/22201 Reisin, Esteban Rodolfo; Scheer, Jurgen; Gravity wave activity in the mesopause region from airglow measurements at El Leoncito; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 66; 6-9; 12-2004; 655-661 1364-6826 CONICET Digital CONICET |
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http://hdl.handle.net/11336/22201 |
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Reisin, Esteban Rodolfo; Scheer, Jurgen; Gravity wave activity in the mesopause region from airglow measurements at El Leoncito; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 66; 6-9; 12-2004; 655-661 1364-6826 CONICET Digital CONICET |
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eng |
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