Lightning Bubbles Caused by Upward Reflectivity Pulses above Precipitation Cores of a Thundercloud
Author:
Affiliation:
1. Institute for Space-Earth Environment Research, Nagoya University
2. National Institute of Information and Communications Technology
3. Osaka University
4. Center for Space Science and Radio Engineering, University of Electro-Communications
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/sola/18/0/18_2022-018/_pdf
Reference16 articles.
1. Calhoun, K. M., D. R. MacGorman, C. L. Ziegler, and M. I. Biggerstaff, 2013: Evolution of lightning activity and storm charge relative to dual-Doppler analysis of a high-precipitation supercell storm. Mon. Wea. Rev., 141, 2199-2223.
2. Dolan, B., and S. A. Rutledge, 2009: A theory-based hydrometeor identification algorithm for X-band polarimetric radars. J. Atmos. Oceanic Technol., 26, 2071-2088.
3. Japan Meteorological Agency, 2013: Outline of the operational numerical weather prediction at the Japan Meteorological Agency. 201 pp (Available online at: https://www.jma.go.jp/jma/jma-eng/jma-center/nwp/outline2013-nwp/index.htm, accessed 30 December 2021).
4. Kouketsu, T., H. Uyeda, T. Ohigashi, M. Oue, H. Takeushi, T. Shinoda, K. Tsuboki, M. Kubo, and K. Muramoto, 2015: A hydrometeor classification method for X-band polarimetric radar: Construction and validation focusing on solid hydrometeors under moist environments. J. Atmos. Oceanic Technol., 32, 2052-2074.
5. Lhermitte, R. M., and P. Krehbiel, 1979: Doppler radar and radio observations of thunderstorms. IEEE Trans. Geosci. Electron., 17, 162-171.
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