Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models
Mesospheric winds observed with a meteor radar at Cariri (7.4° S, 36.5° W), Brazil, during the period of July 2004 to June 2005, show a clear semiannual oscillation known as the Mesospheric Semiannual Oscillation (MSAO), which maximizes in the zonal mean wind mainly at 82 km, with...
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doaj-742de5187a6b450db2a24ba6753f46262020-11-24T23:23:55ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-03-012648549710.5194/angeo-26-485-2008Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing modelsR. A. Buriti0R. A. Buriti1W. K. Hocking2P. P. Batista3A. F. Medeiros4B. R. Clemesha5Departamento de Fisica, Universidade Federal de Campina Grande, Campina Grande, PB, 58109-970, Brazilnow at: Department of Physics and Astronomy, UWO, London, CanadaDepartment of Physics and Astronomy, University of Western Ontario, London, Ontario, CanadaInstituto Nacional de Pesquisas Espaciais (INPE), Sao Jose dos Campos, SP, BrazilDepartamento de Fisica, Universidade Federal de Campina Grande, Campina Grande, PB, 58109-970, BrazilInstituto Nacional de Pesquisas Espaciais (INPE), Sao Jose dos Campos, SP, BrazilMesospheric winds observed with a meteor radar at Cariri (7.4° S, 36.5° W), Brazil, during the period of July 2004 to June 2005, show a clear semiannual oscillation known as the Mesospheric Semiannual Oscillation (MSAO), which maximizes in the zonal mean wind mainly at 82 km, with amplitude decreasing with height. Maximum westward winds for the MSAO occurred in March and September. The meridional wind, on the other hand, presented a clear annual variation maximizing in December. On average, the amplitude of the meridional MSAO was smaller than the zonal MSAO component. Comparison with models shows on occasions that there are significant differences between the observed winds and the CIRA (Cospar International Reference Atmosphere) and HWM93 (Horizontal Wind Model) models. In addition, diurnal and semidiurnal parameters were calculated and compared to the GSWM model. Other results observed during one year of data are presented in this work.https://www.ann-geophys.net/26/485/2008/angeo-26-485-2008.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
R. A. Buriti R. A. Buriti W. K. Hocking P. P. Batista A. F. Medeiros B. R. Clemesha |
spellingShingle |
R. A. Buriti R. A. Buriti W. K. Hocking P. P. Batista A. F. Medeiros B. R. Clemesha Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models Annales Geophysicae |
author_facet |
R. A. Buriti R. A. Buriti W. K. Hocking P. P. Batista A. F. Medeiros B. R. Clemesha |
author_sort |
R. A. Buriti |
title |
Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models |
title_short |
Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models |
title_full |
Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models |
title_fullStr |
Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models |
title_full_unstemmed |
Observations of equatorial mesospheric winds over Cariri (7.4° S) by a meteor radar and comparison with existing models |
title_sort |
observations of equatorial mesospheric winds over cariri (7.4° s) by a meteor radar and comparison with existing models |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2008-03-01 |
description |
Mesospheric winds observed with a meteor radar at Cariri (7.4° S,
36.5° W), Brazil, during the period of July 2004 to June 2005, show a clear
semiannual oscillation known as the Mesospheric Semiannual Oscillation
(MSAO), which maximizes in the zonal mean wind mainly at 82 km, with
amplitude decreasing with height. Maximum westward winds for the MSAO
occurred in March and September. The meridional wind, on the other hand,
presented a clear annual variation maximizing in December. On average, the
amplitude of the meridional MSAO was smaller than the zonal MSAO component.
Comparison with models shows on occasions that there are significant
differences between the observed winds and the CIRA (Cospar International
Reference Atmosphere) and HWM93 (Horizontal Wind Model) models. In addition,
diurnal and semidiurnal parameters were calculated and compared to the GSWM
model. Other results observed during one year of data are presented in this
work. |
url |
https://www.ann-geophys.net/26/485/2008/angeo-26-485-2008.pdf |
work_keys_str_mv |
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