Positive Cloud-to-Ground Lightning Characteristics in the Eyewall of Typhoon Faxai (2019) Observed by Tokyo Lightning Mapping Array

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  • SAKURAI Namiko
    National Research Institute for Earth Science and Disaster Resilience (NIED), Tsukuba, Japan
  • FUDEYASU Hironori
    Graduate School of Education, Yokohama National University, Yokohama, Japan Typhoon Science and Technology Research Center, Yokohama National University, Yokohama, Japan
  • KREHBIEL Paul R.
    New Mexico Institute of Mining and Technology, New Mexico, USA
  • THOMAS Ronald J.
    New Mexico Institute of Mining and Technology, New Mexico, USA
  • RISON William
    New Mexico Institute of Mining and Technology, New Mexico, USA
  • RODEHEFFER Daniel
    New Mexico Institute of Mining and Technology, New Mexico, USA

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  • Tokyo LMAで観測された2019年台風15号の壁雲における正極性落雷の特徴

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Abstract

<p>Although a number of studies have been conducted of the lightning activity in hurricanes and typhoons, little information has been obtained on the three-dimensional (3-D) structure of the lightning, or how it is related to the precipitation structures within the storms. Here, we utilize observational data from the 3-D Tokyo Lightning Mapping Array (Tokyo LMA), a Japan Meteorological Agency C-band Doppler radar, and the Japanese Lightning Detection Network (JLDN) to conduct a study of the lightning activity during Typhoon Faxai (2019) in comparison with the storm's precipitation structure. This is done for the dissipating stage of the typhoon, when the eyewall was well within the range of the instruments and undergoing a surge in lightning activity. Of particular interest in the surge was the occurrence of numerous positive cloud-to-ground (+CG) lightning flashes. Detailed study of the Tokyo LMA and JLDN data shows that, out of 52 flashes during the surge, 29 flashes or 56 % produced positive strokes to ground, an unheard of number considering that, from the lightning and 3-D radar structures, the storm appeared to be normally electrified, and under such circumstances would produce negative rather than positive strokes to ground. It also focuses attention on the question of how +CGs are produced in tropical cyclones in the first place. Based on a lack of −CG strokes and the LMA observations showing that the +CG strokes are produced mid-way or toward the end of normal polarity intracloud (IC) flashes, it appears that the dissipating storm cells have a depleted or horizontally sheared mid-level negative charge, such that an IC flash propagating into and through upper positive storm charge effectively funnels a steadily increasing amount of positive charge into the mid-level initiation region, eventually causing the positive breakdown of the IC flash to turn downward toward ground, producing a +CG stroke.</p>

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