日本地球惑星科学連合2019年大会

講演情報

[E] 口頭発表

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) 10:45 〜 12:15 104 (1F)

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)、座長:宮本 佳明伊藤 耕介(琉球大学)

10:45 〜 11:15

[AAS02-07] A change in the inner-core structure of Typhoon Trami (2018) as observed through upper-tropospheric aircraft reconnaissance of T-PARCII

★Invited Papers

*山田 広幸1坪木 和久2篠田 太郎2久保田 尚之3高橋 幸弘3長浜 則夫4清水 健作4大東 忠保5伊藤 耕介1山口 宗彦6中澤 哲夫6 (1.琉球大学、2.名古屋大学、3.北海道大学、4.明星電気、5.防災科学技術研究所、6.気象庁気象研究所)

キーワード:航空機観測、台風、北西太平洋

Upper-tropospheric aircraft reconnaissance with dropsonde deployment using a Gulfstream-II aircraft was carried out for the inner core of Typhoon Trami on four successive days since 25 September 2018. According to the JMA best track, the central pressure reached its minimum value of 915 hPa on the first day and was subsequently maintained at 950 hPa for three days. Using dropsonde data, this study examined the change in the inner-core structure associated with the intensity change. Based on satellite imagery, this intensity change was associated with the rapid expansion of the eye (with radius increasing from 35 to 90 km) and the gradual increase in the eyewall cloud-top height. A composite analysis of dropsonde profiles in the radius-height domain on each day revealed a change in the flow structure, with the decrease (increase) in the tangential wind component near the radius of 40 km (120 km). This caused an increase in the radial gradient of angular momentum, corresponding to an increase in inertial stability. These results suggest that this typhoon underwent the structural change similar to eyewall replacement cycle while the central pressure was maintained.



Acknowledgements: This work was supported by JSPS KAKENHI Grant Numbers JP16H06311, JP16H04053, JP18H03805, and the Science and Technology Research Partnership for Sustainable Development (SATREPS) Understanding Lightning and Thunderstorm (ULAT) project.