TY - JOUR
T1 - Rocktsonde observations of the middle atmosphere dynamics at uchinoura(31°N,131°E) during the DYANA campaign. Part I
T2 - Outline of experiments and background conditions
AU - Yamanaka, M. D.
AU - Murayama, Y.
AU - Tsuda, T.
AU - Nakamura, T.
AU - Fukao, S.
AU - Kato, S.
AU - Oyama, K. I.
AU - Kanzawa, H.
AU - Schmidlin, F. J.
AU - Bittner, M.
PY - 1992
Y1 - 1992
N2 - We describe in this paper preliminary results on the characteristics of the wind velocity and temperature profiles obtained through rocketsonde measurements during the DYANA campaign. The wind velocity profiles in the height region of 20-90km, obtained with the rocketsondes, were compared with the results simultaneously observed with the MU (middle and upper atmosphere) radar at 60-100km. The profiles were consistent with each other up to 80km, when they were smoothed out for a height range of 8km. While for wind velocity fluctuations with vertical scales of a few km, the rocketsonde results showed significantly larger amplitudes than those obtained with the MU radar above 60km. Consideration of the vertical wavenumber spectra of the wind velocity fluctuations suggested that the maximum height range of the rocketsonde profile, by which the gravity wave characteristics can be delineated, seemed to be limited only up to about 60km. The background zonal winds were westward in the stratosphere, but they exhibited large time variations, coinciding with a minor stratospheric sudden warming. The temperature profiles also indicated great variability near the stratopause and in the mesosphere, probably due to the effect of the enhanced activity of planetary waves.
AB - We describe in this paper preliminary results on the characteristics of the wind velocity and temperature profiles obtained through rocketsonde measurements during the DYANA campaign. The wind velocity profiles in the height region of 20-90km, obtained with the rocketsondes, were compared with the results simultaneously observed with the MU (middle and upper atmosphere) radar at 60-100km. The profiles were consistent with each other up to 80km, when they were smoothed out for a height range of 8km. While for wind velocity fluctuations with vertical scales of a few km, the rocketsonde results showed significantly larger amplitudes than those obtained with the MU radar above 60km. Consideration of the vertical wavenumber spectra of the wind velocity fluctuations suggested that the maximum height range of the rocketsonde profile, by which the gravity wave characteristics can be delineated, seemed to be limited only up to about 60km. The background zonal winds were westward in the stratosphere, but they exhibited large time variations, coinciding with a minor stratospheric sudden warming. The temperature profiles also indicated great variability near the stratopause and in the mesosphere, probably due to the effect of the enhanced activity of planetary waves.
UR - https://www.scopus.com/pages/publications/0027097236
UR - https://www.scopus.com/pages/publications/0027097236#tab=citedBy
U2 - 10.5636/jgg.44.995
DO - 10.5636/jgg.44.995
M3 - Article
AN - SCOPUS:0027097236
SN - 0022-1392
VL - 44
SP - 995
EP - 1007
JO - Journal of geomagnetism and geoelectricity
JF - Journal of geomagnetism and geoelectricity
IS - 11
ER -