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) 15:30 〜 17:00 104 (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:金田 幸恵(名古屋大学)、宮本 佳明

16:00 〜 16:15

[AAS02-14] Binary interaction between TC Chanthu (2016) and a nearby cold low

*伊藤 耕介1比嘉 未雅1Chan Johnny2 (1.琉球大学、2.City University of Hong Kong)

キーワード:tropical cyclone、Fujiwhara effect、track forecast

Tropical cyclone (TC) Chanthu (2016) caused the heavy rainfall and strong wind on Hokkaido Prefecture, Japan. However, this was one of the "busted" cases in which the track forecast error reached up to 900 km in a 72-h forecast by the Regional Specialized Meteorological Center (RSMC) Tokyo. In fact, the re-forecast experiment with Japan Meterological Agency Non-Hydrostatic Model (JMA-NHM) that employed Kain-Fritsch scheme as a convective parameterization correctly captured the observed northward translation speed of TC Chanthu, while the JMA Global Spectral Model (JMA-GSM) and JMA-NHM that employed Arakawa-Schubert scheme failed to predict the accurate northward translation speed. The mesoscale analysis showed that there was a cold low located at 200km west of TC Chanthu (2016). With Kain-Frische scheme, the binary interaction between TC Chanthu and the nearby cold low was reproduced so that it contributed the faster translation to the north as consistent with the best track. In contrast, the binary interaction was not reproduced in the simulations with Arakawa-Schubert scheme because a triggered large-scale convection made TC Chanthu and the nearby cold low merged. It exemplifies that the reproduction of fine-scale features diminishes "busted" cases, which contributes to the disaster prevention and mitigation.