Articles | Volume 31, issue 5
Ann. Geophys., 31, 845–858, 2013
Ann. Geophys., 31, 845–858, 2013

Regular paper 15 May 2013

Regular paper | 15 May 2013

Studies of gravity wave propagation in the mesosphere observed by MU radar

H. Y. Lue1, F. S. Kuo2, S. Fukao3, and T. Nakamura3 H. Y. Lue et al.
  • 1Department of Physics, Fu Jen University, Hsin Chuang, Taiwan
  • 2Department of Electro-Optical Engineering, Vanung University, Chung-Li, Taiwan
  • 3Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan

Abstract. Mesospheric data were analyzed by a composite method combining phase and group velocity tracing technique and the spectra method of Stokes parameter analysis to obtain the propagation parameters of atmospheric gravity waves (AGW) in the height ranges between 63.6 and 99.3 km, observed using the MU radar at Shigaraki in Japan in the months of November and July in the years 1986, 1988 and 1989. The data of waves with downward phase velocity and the data of waves with upward phase velocity were independently treated. First, the vertical phase velocity and vertical group velocity as well as the characteristic wave period for each wave packet were obtained by phase and group velocity tracing technique. Then its horizontal wavelength, intrinsic wave period and horizontal group velocity were obtained by the dispersion relation. The intrinsic frequency and azimuth of wave vector of each wave packet were checked by Stokes parameters analysis. The results showed that the waves with intrinsic periods in the range 30 min–4.5 h had horizontal wavelength ranging from 25 to 240 km, vertical wavelength from 2.5 to 12 km, and horizontal group velocities from 15 to 60 m s−1. Both upward moving wave packets and downward moving wave packets had horizontal group velocities mostly directed in the sector between directions NNE (north-north-east) and SEE in the month of November, and mostly in the sector between directions NW and SWS in the month of July. Comparing with mean wind directions, the gravity waves appeared to be more likely to propagate along with mean wind than against it. This apparent prevalence for downstream wave packets was found to be caused by a systematic filtering effect existing in the process of phase and group velocity tracing analysis: A significant portion of upstream wave packets might have been Doppler shifted out of the vertical range in phase and group velocity tracing analysis.