Vertical propagation of gravity waves determined from zenith observations of airglow
From our growing data base of OH and O2 airglow intensity and temperature measurements at lower mid-latitudes, gravity wave information has been extracted by time series spectral analysis. According to existing theories, the amplitude and phase relationships between intensities and rotational temper...
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| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
| Publicado: |
2001
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| Acceso en línea: | Registro en Scopus DOI Handle Registro en la Biblioteca Digital |
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| LEADER | 06489caa a22006497a 4500 | ||
|---|---|---|---|
| 001 | PAPER-20570 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205159.0 | ||
| 008 | 190411s2001 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0034817145 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a ASRSD | ||
| 100 | 1 | |a Reisin, E.R. | |
| 245 | 1 | 0 | |a Vertical propagation of gravity waves determined from zenith observations of airglow |
| 260 | |c 2001 | ||
| 270 | 1 | 0 | |m Reisin, E.R.; Inst. Astron. Fisica del Espacio, CONICET, Ciudad Universitaria, Buenos Aires 1428, Argentina |
| 506 | |2 openaire |e Política editorial | ||
| 504 | |a Gavrilov, N.M., Fukao, S., Nakamura, T., Tsuda, T., Statistical analysis of gravity waves observed with the middle and upper atmosphere radar in the middle atmosphere. 2. Waves propagated in different directions (1997) J. Geophys. Res, 102, pp. 13433-13440 | ||
| 504 | |a Hines, C.O., Tarasick, D.W., On the detection and utilization of gravity waves in airglow studies (1987) Planet. Space Sci, 35, pp. 851-866 | ||
| 504 | |a Hines, C.O., Tarasick, D.W., Airglow response to vertically standing gravity waves (1994) Geophys. Res. Lett, 21, pp. 2729-2732 | ||
| 504 | |a Reisin, E.R., Scheer, J., Characteristics of atmospheric waves in the tidal period range derived from zenith observations of O2b(0-1) atmospheric and OH(6-2) airglow at lower mid-latitudes (1996) J. Geophys. Res, 101, pp. 21223-21232 | ||
| 504 | |a Reisin, E.R., Scheer, J., Nuevos Avances en la Extracción de Parámetros de Ondas Atmosféricas Utilizando Temperaturas Rotacionales de las Emisiones de OH y O2 (1996) 4a Conferencia Latinoamericana De Geofísica Espacial (COLAGE), , Tucuman, April 22-26 | ||
| 504 | |a Scheer, J., Reisin, E.R., Espy, J.P., Bittner, M., Graef, H.-H., Offermann, D., Ammosov, P.P., Ignatyev, V.M., Large-scale structures in hydroxyl rotational temperatures during DYANA (1994) J. Atmos. Terr. Phys, 56, pp. 1701-1715 | ||
| 504 | |a Scheer, J., Reisin, E.R., Unusually low airglow intensities in the Southern Hemisphere Midlatitude Mesopause Region (2000) Earth Planets and Space, 52, pp. 261-266 | ||
| 504 | |a Scheer, J., Reisin, E.R., Refinements of a classical technique of airglow spectroscopy (2001) Adv. Space Res, , in press | ||
| 504 | |a Swenson, G.R., Gardner, C.S., Analytical models for the responses of the mesospheric OH* and Na to atmospheric gravity waves (1998) J. Geophys. Res, 103, pp. 6271-6294 | ||
| 504 | |a Takahashi, H., Batista, P.P., Buriti, R.A., Gobbi, D., Nakamura, T., Tsuda, T., Fukao, S., Response of the airglow OH emission, temperature and mesopause wind to the atmospheric wave propagation over Shigaraki, Japan (1999) Earth Planets and Space, 51, pp. 863-875 | ||
| 504 | |a Tarasick, D.W., Shepherd, G.G., Effects of gravity waves on complex airglow chemistries. 1. O2(b1∑+g) emission (1992) J. Geophys. Res, 97, pp. 3185-3193 | ||
| 504 | |a Tarasick, D.W., Shepherd, G.G., Effects of gravity waves on complex airglow chemistries. 2. OH emission (1992) J. Geophys. Res, 97, pp. 3195-3208 | ||
| 504 | |a Walterscheid, R.L., Hecht, J.H., Vincent, R.A., Reid, I.M., Woithe, J., Hickey, M.P., Analysis and interpretation of airglow and radar observations of quasi-monochromatic gravity waves in the upper mesosphere and lower thermosphere over Adelaide, Australia (35°S, 138°E) (1999) J. Atmos. Solar-Terr. Phys, 61, pp. 461-478 | ||
| 504 | |a Walterscheid, R.L., Hecht, J.H., Djuth, F.T., Tepley, C.A., Evidence of reflection of a long-period gravity wave in observations of the nightglow over Arecibo on May 8-9, 1989 (2000) J. Geophys. Res, 105, pp. 6927-6934 | ||
| 520 | 3 | |a From our growing data base of OH and O2 airglow intensity and temperature measurements at lower mid-latitudes, gravity wave information has been extracted by time series spectral analysis. According to existing theories, the amplitude and phase relationships between intensities and rotational temperatures for a given airglow emission contain information about vertical wave propagation. A wide but clearly non-random distribution of phase shifts between intensity and temperature is observed. Cases of 180°, often cited in the literature, are definitely exceptions, here. For observed periods between about ten minutes and three hours, 30% of the waves at 95 km, and 40% at 87 km propagate downward. This signals the importance of wave reflection in the mesopause region. © 2001 COSPAR. Published by Elsevier Science Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica, 07-00000-01818/ PICT ‘97-1818, PIP 4554/96, PMP PICT 0137 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: ACKNOWLEDGEMENTS The authors gratefully acknowledge the active support by the staff of Complejo Astronomic0 El Leoncito which has made the observational success of the recent years possible. This work was partially funded by CONICET and ANPCyT grants PMP PICT 0137, PIP 4554/96, and 07-00000-01818/ PICT ‘97-1818. | ||
| 593 | |a Instituto de Astronomía y Física del Espacio, CONICET, Ciudad Universitaria, 1428 Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a GRAVITY WAVES |
| 690 | 1 | 0 | |a PHASE SHIFT |
| 690 | 1 | 0 | |a REFLECTION |
| 690 | 1 | 0 | |a TIME SERIES ANALYSIS |
| 690 | 1 | 0 | |a VERTICAL WAVE PROPAGATION |
| 690 | 1 | 0 | |a ZENITH OBSERVATIONS |
| 690 | 1 | 0 | |a SPACE RESEARCH |
| 690 | 1 | 0 | |a AIRGLOW |
| 690 | 1 | 0 | |a AMPLITUDE |
| 690 | 1 | 0 | |a GRAVITY WAVE |
| 690 | 1 | 0 | |a SPECTRAL ANALYSIS |
| 690 | 1 | 0 | |a WAVE PROPAGATION |
| 700 | 1 | |a Scheer, J. | |
| 773 | 0 | |d 2001 |g v. 27 |h pp. 1743-1748 |k n. 10 |p Adv. Space Res. |x 02731177 |w (AR-BaUEN)CENRE-3577 |t Advances in Space Research | |
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| 856 | 4 | 0 | |u https://doi.org/10.1016/S0273-1177(01)00313-1 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_02731177_v27_n10_p1743_Reisin |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02731177_v27_n10_p1743_Reisin |y Registro en la Biblioteca Digital |
| 961 | |a paper_02731177_v27_n10_p1743_Reisin |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a VARI | ||