Special Issue: Dynamics and Structure of the Mesopause Region (DYSMER)
- Article
- Published:
QBO effects on the diurnal tide in the upper atmosphere
Earth, Planets and Space volume 51, pages 571–578 (1999)
Abstract
We report on a series of numerical experiments conducted with the global-scale wave model (GSWM) and designed to investigate the effects of the quasi-biennial oscillation (QBO) on the migrating diurnal tide. Our results indicate that the diurnal tidal response in the upper mesosphere and lower thermosphere (MLT) is significantly affected by the QBO in zonal mean zonal winds, but largely insensitive to the QBO in stratospheric ozone. We discuss the variable mean wind results in light of previous analytic attempts to describe the diurnal tide in the presence of mean winds and dissipation. Our calculations do not explain the interannual tidal variations observed by the High Resolution Doppler Interferometer (HRDI) on the Upper Atmosphere Research Satellite (UARS).
References
Aso, T., T. Y. Nonoyama, and S. Kato, Numerical simulation of semidiurnal atmospheric tides, J. Geophys. Res., 86, 11,388–11,400, 1981.
Batten, E. S., Wind systems in the mesosphere and lower ionosphere, J. Meteorol., 18, 283–291, 1961.
Burrage, M. D., M. E. Hagan, W. R. Skinner, D. L. Wu, and P. B. Hays, Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM, Geophys. Res. Lett., 22, 2641–2644, 1995.
Burrage, M. D., R. A. Vincent, H. G. Mayr, W. R. Skinner, N. F. Arnold, and P. B. Hays, Long-term variability in the equatorial mesosphere and lower thermosphere zonal wind, J. Geophys. Res., 101, 12,847–12,854, 1996.
Ekanayake, E. M. P., T. Aso, and S. Miyahara, Background wind effect on propagation of nonmigrating diurnal tides in the middle atmosphere, J. Atmos. Sol.-Terr. Phys., 59, 401–429, 1997.
Forbes, J. M., Atmospheric tides, 1, Model description and results for the solar diurnal component, J. Geophys. Res., 87, 5222–5240, 1982.
Forbes, J. M. and M. E. Hagan, Diurnal propagating tide in the presence of mean winds and dissipation: A numerical investigation, Planet. Space Sci., 36, 579–590, 1988.
Forbes, J. M. and F. Vial, Monthly simulation of the solar semidiurnal tide in the mesosphere and lower thermosphere, J. Atmos. Terr. Phys., 51, 649–661, 1989.
Forbes, J. M. and R. A. Vincent, Effects of mean winds and dissipation on the diurnal propagating tide: An analytic approach, Planet. Space Sci., 37, 197–209, 1989.
Garcia, R. R., T. J. Dunkerton, R. S. Lieberman, and R. A. Vincent, Climatology of the semiannual oscillation of the tropical middle atmosphere, J. Geophys. Res., 102, 26,019–26,032, 1997.
Geller, M. A., B. V. Khattatov, V. A. Yudin, and M. E. Hagan, Modeling the diurnal tide with dissipation derived from UARS/HRDI measurements, Ann. Geophys., 15, 1198–1204, 1997.
Groves, G. V., Hough components of water vapor heating, J. Atmos. Terr. Phys., 44, 281–290, 1982.
Groves, G. V., A global reference atmosphere from 18 to 80 km, AFGL Report TR-85-0129, 1985.
Groves, G. V., Final scientific report, AFOSR Report 84-0045, 1987.
Hagan, M. E., Comparative effects of migrating solar sources on tidal signatures in the middle and upper atmosphere, J. Geophys. Res., 101, 21,213–21,222, 1996.
Hagan, M. E., F. Vial, and J. M. Forbes, Evidence of variability in upward propagating semidiurnal tides due to effects of QBO in the lower atmosphere, J. Atmos. Terr. Phys., 54, 1465–1474, 1992.
Hagan, M. E., J. M. Forbes, and F. Vial, On modeling migrating solar tides, Geophys. Res. Lett., 22, 893–896, 1995.
Hagan, M. E., M. D. Burrage, J. M. Forbes, J. Hackney, W. J. Randel, and X. Zhang, GSWM-98: Results for migrating solar tides, J. Geophys. Res., 104, 6813–6828, 1999.
Hedin, A. E., Extension of the MSIS thermosphere model into the middle and lower atmosphere, J. Geophys. Res., 96, 1159–1172, 1991.
Hines, C. O., The upper atmosphere in motion, in Geophys. Mono., No. 18, 1027 pp., American Geophysical Union, Washington, DC, 1974.
Hines, C. O., Latitudinal variation of tidal dissipation and upward propagation, Planet. Space Sci., 37, 669–683, 1989.
Kantor, A. J., and A. E. Cole, Zonal and meridional winds to 120 kilometers, J. Geophys. Res., 69, 5131–5140, 1964.
Lindzen, R. S., Equatorial planetary waves in shear: Part II, J. Atmos. Sci., 29, 1452–1463, 1972.
Lindzen, R. S. and S. S. Hong, Effects of mean winds and horizontal temperature gradients on solar and lunar semidiurnal tides in the atmosphere, J. Atmos. Sci., 31, 1421–1466, 1974.
Mayr, H. G., J. G. Mengel, C. O. Hines, K. L. Chan, N. F. Arnold, C. A. Reddy, and H. S. Porter, The gravity wave Doppler spread theory applied in a numerical spectral model of the middle atmosphere, 2, Equatorial oscillations, J. Geophys. Res., 102, 26,093–26,105, 1997.
Meyer, C. K., Gravity wave interactions with the diurnal propagating tide, J. Geophys. Res., in press, 1999.
Murgatroyd, R. J., Winds in the mesosphere and lower thermosphere, Proc. Roy. Soc. London, A288, 575–589, 1965.
Murphy, C., Seasonal variations of ionospheric wind over Barbados, J. Geophys. Res., 74, 339–367, 1969.
Portnyagin, Yu. I. and T. V. Solov’eva, An empirical model of the meridional wind in the mesopause-lower thermosphere, Part 1, A mean monthly empirical model, Russian J. Met. and Hydr., 10, 28–35, 1992a.
Portnyagin, Yu. I. and T. V. Solov’eva, An empirical model of the meridional wind in the mesopause/lower thermosphere, Part 2, Height-latitude features of basic components of meridional wind seasonal variations, Russian J. Met. and Hydr., 11, 29–36, 1992b.
Randel, W. J., Global atmospheric circulation statistics, 1000-1 mb, National Center for Atmospheric Research Technical Note 366, 1992.
Randel, W. J. and F. Wu, Insolation of ozone QBO in SAGE II data by singular-value decomposition, J. Atmos. Sci., 53, 2546–2559, 1996.
Randel, W. J., F. Wu, J. M. Russell, III A. Roche, and J. Waters, Seasonal cycles and QBO variations in stratospheric CH4and H2O observed in UARS HALOE data, J. Atmos. Sci., 55, 163–185, 1998.
Richmond, A. D., Energy relations of atmospheric tides and their significance to approximate methods of solutions of tides with dissipative forces, J. Atmos. Sci., 32, 980–987, 1975.
Sassi, F. and R. R. Garcia, A one-dimensional model of the semiannual oscillation driven by convectively forced gravity waves, J. Atmos. Sci., 51, 3167–3182, 1994.
Strobel, D. F., Parameterization of the atmospheric heating rate from 15 to 120 km due to O2 and O3 absorption of solar radiation, J. Geophys. Res., 83, 6225–6230, 1978.
Vial, F., Numerical simulations of atmospheric tides, J. Geophys. Res., 91, 8955–8969, 1986.
Vincent, R. A., S. Kovalam, D. C. Fritts, and J. R. Isler, Long-term MF radar observations of solar tides in the low-latitude mesosphere: Interannual variability and comparisons with the GSWM, J. Geophys. Res., 103, 8667–8683, 1998.
Walterscheid, R. J., J. G. de Vore, and S. V. Venkateswaran, Influence of mean zonal motion and meridional temperature gradients on the solar semidiurnal tide: A revised spectral study with improved heating rates, J. Atmos. Sci., 37, 455–470, 1980.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Hagan, M.E., Burrage, M.D., Forbes, J.M. et al. QBO effects on the diurnal tide in the upper atmosphere. Earth Planet Sp 51, 571–578 (1999). https://doi.org/10.1186/BF03353216
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1186/BF03353216