Small ScaleTurbulence Observed Simultaneously by Radiosondes and the MU Radar
| Autor: | Wilson, Richard, Luce, Hubert, Hashiguchi, H., Dalaudier, Francis, Fukao, F., Nakajo, F., Shibagaki, F., Yabuki, F., Furumoto, F. |
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| Přispěvatelé: | TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de sondages électromagnétiques de l'environnement terrestre (LSEET), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS), Research Institute for Sustainable Humanosphere (RISH), Kyoto University [Kyoto], STRATO - LATMOS, Department of Electrical, Electronics and Computer Engineering [Fukui], Fukui University of Technology, Osaka Electro-Communication University, Osaka University [Osaka], Kyoto University |
| Jazyk: | angličtina |
| Rok vydání: | 2012 |
| Předmět: | |
| Zdroj: | 9th International Symposium on Tropospheric Profiling (ISTP) 9th International Symposium on Tropospheric Profiling (ISTP), Sep 2012, L'Aquila, Italy. 3 p |
| Popis: | International audience; A Japanese-French field campaign devoted to study small-scale turbulence and instabilities in the lower atmosphere was conducted in September 2011 for three weeks at Shigaraki MU observatory (34.85N, 136.15E; Japan). The VHF MU radar was operated in range imaging mode [e.g. 1] for turbulence observations at high temporal ( 25 s) and high range (typically 30 m) resolutions. In addition, 59 balloons instrumented with RS92G Vaisala radiosondes were succesfully launched during the campaign when the radar was operated. Reference [2] showed that turbulence can be detected from raw vertical profiles of temperature measured from standard radiosoundings through the detection of overturns using the so-called Thorpe analysis [3]. In the present work, we shall present some comparison results between radiosonde and MU radar data. |
| Databáze: | OpenAIRE |
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