日本地球惑星科学連合2019年大会

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS02] 台風研究の新展開~過去・現在・未来

2019年5月30日(木) 13:45 〜 15:15 ポスター会場 (幕張メッセ国際展示場 8ホール)

コンビーナ:金田 幸恵(名古屋大学宇宙地球環境研究所)、和田 章義(気象研究所台風・災害気象研究部)、伊藤 耕介(琉球大学)、宮本 佳明(慶應義塾大学 環境情報学部)

[AAS02-P01] Numerical study on lightning frequency in a tropical cyclone

*佐藤 陽祐1,3宮本 佳明2,3富田 浩文3 (1.名古屋大学工学研究科、2.慶應大学環境情報学部、3.理化学研究所計算科学研究センター)

キーワード:台風、雷

This study investigates frequency of lightning in each stage of lifecycle of tropical cyclone (TC) using the next generation weather and climate library called Scalable Computing for Advanced Library and Environment (SCALE; Sato et al. 2015, Nishizawa et al. 2015). Lightning component was developed and implemented into SCALE in this study. An idealized experiment based on an experimental setup of Miyamoto and Takemi (2013) was conducted by SCALE coupled with lightning component. The results of the simulation indicate that the lightning frequency is maximum before rapid intensification (RI) of TC, which supports the report of Price et al. (2009) derived from satellite observation. The frequency of lightning decreases after RI and it keeps small until the TC reaches steady state. Our analyses elucidate that the dependency of the lightning frequency upon the developing stage of TC is originated from the type of convection dominating at each growth stage. Before the RI, the convection generated by consuming convective available potential energy (CAPE) transport hydrometeors upward, and the charge split and the lightning frequently occur. During the steady state, the hydrometeors are mainly transported by the fast rotating flow in the simulated TC, which resulted in the weak charge split and small frequency of lightning.