書誌事項
- 公開日
- 1994-02
- DOI
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- 10.1175/1520-0426(1994)011<0050:oottfw>2.0.co;2
- 公開者
- American Meteorological Society
この論文をさがす
説明
Abstract 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. Wavelike temperature fluctuations with a dominant period of 6–8 h clearly showed downward phase progression and a π/2 p...
収録刊行物
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- Journal of Atmospheric and Oceanic Technology
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Journal of Atmospheric and Oceanic Technology 11 (1), 50-62, 1994-02
American Meteorological Society
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詳細情報 詳細情報について
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- CRID
- 1361137043443383168
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- ISSN
- 15200426
- 07390572
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- データソース種別
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- Crossref
- OpenAIRE