The semidiurnal tide for individual nights derived consistently from O 2 and OH intensities and temperatures
The semidiurnal tide is studied with 159 special cases from the large airglow database acquired at El Leoncito (31.8ºS, 69.3ºW). These cases correspond to nights which exhibit similar periods in the temperature and intensity variations of the OH(6-2) and O 2 b(0–1) emissions. We find that all the pe...
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Elsevier Ltd
2019
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LEADER | 10051caa a22008417a 4500 | ||
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001 | PAPER-25585 | ||
003 | AR-BaUEN | ||
005 | 20230518205740.0 | ||
008 | 190410s2019 xx ||||fo|||| 00| 0 eng|d | ||
024 | 7 | |2 scopus |a 2-s2.0-85061524341 | |
040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
100 | 1 | |a Reisin, E.R. | |
245 | 1 | 4 | |a The semidiurnal tide for individual nights derived consistently from O 2 and OH intensities and temperatures |
260 | |b Elsevier Ltd |c 2019 | ||
270 | 1 | 0 | |m Reisin, E.R.; Instituto de Astronomía y Física del Espacio, Ciudad Universitaria, C.C. 67 Suc. 28, Argentina; email: ereisin@iafe.uba.ar |
506 | |2 openaire |e Política editorial | ||
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504 | |a Smith, S.M., Baumgardner, J., Mertens, C.J., Russell, J.M., Mlynczak, M.G., Mendillo, M., Mesospheric OH temperatures: simultaneous ground-based and SABER OH measurements over Millstone hill (2010) Adv. Space Res., 45, pp. 239-246 | ||
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504 | |a Takahashi, H., Gobbi, D., Batista, P.P., Melo, S.M.L., Teixeira, N.R., Buriti, R.A., Dynamical influence on the equatorial airglow observed from the South American sector (1998) Adv. Space Res., 21, pp. 817-825 | ||
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520 | 3 | |a The semidiurnal tide is studied with 159 special cases from the large airglow database acquired at El Leoncito (31.8ºS, 69.3ºW). These cases correspond to nights which exhibit similar periods in the temperature and intensity variations of the OH(6-2) and O 2 b(0–1) emissions. We find that all the periods (except one) are between 9 and 15.5 h. The phase distributions of these cases are narrow enough to ensure the identification as the semidiurnal tide, and their progression with altitude is consistent with downward phase propagation. The mean temperature amplitudes are large for both emissions. We obtain new values for Krassovsky's ratio including its phase. The vertical wavelength is determined independently for each emission using the relation suggested by the Hines and Tarasick theory. Mean vertical wavelengths derived for O 2 are longer than those for OH. The longest monthly mean wavelengths are observed from May to August. The mean ratio of temperature amplitudes between the two emissions corresponds to moderate wave attenuation during the upward propagation of the tide. © 2019 Elsevier Ltd |l eng | |
536 | |a Detalles de la financiación: PIP 11220130100439CO | ||
536 | |a Detalles de la financiación: PICT-2016-0221 | ||
536 | |a Detalles de la financiación: We gratefully acknowledge the technical support and many helpful interventions over the many years by the CASLEO staff. Partial funding by the Argentine CONICET PUE-IAFE and PIP 11220130100439CO , and the Argentine ANPCyT PICT-2016-0221 is acknowledged. We also thank the two anonymous reviewers for their suggestions and helpful criticism. Appendix A | ||
593 | |a Instituto de Astronomía y Física del Espacio, CONICET - Universidad de Buenos Aires, Buenos Aires, Argentina | ||
690 | 1 | 0 | |a AIRGLOW |
690 | 1 | 0 | |a MESOPAUSE REGION |
690 | 1 | 0 | |a SEMIDIURNAL TIDE |
690 | 1 | 0 | |a VERTICAL WAVELENGTH |
690 | 1 | 0 | |a EARTH ATMOSPHERE |
690 | 1 | 0 | |a AIRGLOW |
690 | 1 | 0 | |a INTENSITY VARIATIONS |
690 | 1 | 0 | |a MEAN TEMPERATURE |
690 | 1 | 0 | |a MESOPAUSE REGION |
690 | 1 | 0 | |a PHASE DISTRIBUTION |
690 | 1 | 0 | |a PHASE PROPAGATION |
690 | 1 | 0 | |a TEMPERATURE AMPLITUDE |
690 | 1 | 0 | |a WAVE ATTENUATION |
690 | 1 | 0 | |a GEOPHYSICS |
700 | 1 | |a Scheer, J. | |
773 | 0 | |d Elsevier Ltd, 2019 |g v. 186 |h pp. 20-27 |p J. Atmos. Sol.-Terr. Phys. |x 13646826 |w (AR-BaUEN)CENRE-5432 |t Journal of Atmospheric and Solar-Terrestrial Physics | |
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856 | 4 | 0 | |u https://doi.org/10.1016/j.jastp.2019.02.002 |y DOI |
856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_13646826_v186_n_p20_Reisin |y Handle |
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963 | |a VARI |