Applying the RASS (radio acoustic sounding system) technique to the MU (middle and upper atmosphere) radar, profiles of both temperature and wind velocity were observed every 90 s in the height range of about 1.5-7.0 km, with a height resolution of 300 m, for about 40 h on 6-8 August 1990. The temperature profiles obtained with RASS agreed well with the virtual temperature derived from radiosonde sounding, where the mean difference between the temperature values was approximately 0.3°C. The observed frequency spectra above about 2.5-km altitude, having an asymptotic slope of -5/3 and approximately 0 for temperature and vertical wind velocity fluctuations, respectively, were reasonably consistent with a model spectrum of gravity waves. But, below 2.5 km, low-frequency components were conspicuously enhanced, especially for vertical wind velocity, presumably affected by convection. -from Authors
CITATION STYLE
Tsuda, T., Adachi, T., Masuda, Y., Fukao, S., & Kato, S. (1994). Observations of tropospheric temperature fluctuations with the MU radar-RASS. Journal of Atmospheric & Oceanic Technology, 11(1), 50–62. https://doi.org/10.1175/1520-0426(1994)011<0050:OOTTFW>2.0.CO;2
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