JpGU-AGU Joint Meeting 2020

Presentation information

[J] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS20] Atmospheric Electricity: Lightning discharges and related physical phenomena

convener:Yasuhide Hobara(Graduate School of Information and Engineering Department of Communication Engineering and Informatics, The University of Electro-Communications)

[MIS20-06] Meteorological conditions for lightning jump associated with downburst and heavy precipitation in Japan inferred from from X-band radar and Himawari-8 satellite data

*Yasuhide Hobara1, Hiroshi Kikuchi1, Risako Aoyagi1, Michael Stock2 (1.Graduate School of Information and Engineering Department of Communication Engineering and Informatics, The University of Electro-Communications, 2.EarthNetworks)

Keywords:total lightning, extreme weather, downburst, heavy precipitation, radar, meteorological satellite

In this paper we have studied characteristics of thunderstorms producing extreme weather events in detail both from ground-based and satellite measurements. We focused on thunderstorms producing downbursts and heavy rains in summer time in Japan. The data from Total lightning continuously monitored by JTLN (Japanese Total Lightning Network) deployed by UEC over Japan were used to identify Lightning Jump (LJ: sudden increase in lightning discharges) before extreme weather occurrence. LJ is suggested to be useful for severe event prediction. The thunderstorm cells were identified and tracked by using the volume scan data from X-band high speed Doppler weather radar, which provides the information on how the thunderstorms evolve both in space and time coordinates. Moreover, Japanese geostationary meteorological satellite (Himawari 8) data from different optical bands were used to identify the meteorological conditions around the target thunderstorm cells such as cloud top height and amount of water vapor in different altitude. Above-mentioned physical parameters from radar and satellite measurements are utilized to understand the in-cloud meteorological conditions generating total LJ such as updraft intensification in the storm cell and extreme weather event onset.