日本地球惑星科学連合2016年大会

講演情報

インターナショナルセッション(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] High performance computing of next generation weather, climate, and environmental sciences using K

2016年5月22日(日) 17:15 〜 18:30 ポスター会場 (国際展示場 6ホール)

コンビーナ:*佐藤 正樹(東京大学大気海洋研究所)、木本 昌秀(東京大学大気海洋研究所)、斉藤 和雄(気象研究所予報研究部)、瀬古 弘(気象研究所)、三好 建正(理化学研究所計算科学研究機構)、田村 哲郎(東京工業大学大学院総合理工学研究科)、新野 宏(東京大学大気海洋研究所海洋物理学部門海洋大気力学分野)、滝川 雅之(独立行政法人海洋研究開発機構)、富田 浩文(理化学研究所計算科学研究機構)、小玉 知央(独立行政法人海洋研究開発機構)

17:15 〜 18:30

[AAS02-P02] Numerical simulations of Typhoon Haiyan in 2013

*和田 章義1沢田 雅洋1 (1.気象研究所台風研究部)

キーワード:Typhoon, Numerical simulation, Sea surface cooling

Typhoon Haiyan in 2013 was among the strongest ever observed for tropical cyclones globally. The typhoon is characterized by fast translation, rapid intensification and extremely intense intensity at such a low latitude. To understand the behavior of the typhoon and to improve the intensity prediction, numerical simulations were performed by a regional coupled atmosphere-wave-ocean model with a horizontal resolution of 2 km. The effect of sea spray was included in the regional coupled model. Even using the model with a horizontal resolution of 2 km, it was difficult to reproduce rapid intensification of the typhoon and the maximum intensity without the effect of sea spray. An issue on the impact of horizontal resolution of numerical models on the simulation will be addressed. The effect of sea spray was confined to the near-surface boundary layer and led the typhoon to intensify more rapidly. The effect of Haiyan-induced sea surface cooling on the maximum intensity was 10 hPa at the maximum due to the fast translation. In order to understand the effect of translation speed on sea surface cooling and resultant maximum intensity of a typhoon, numerical simulations were performed for Typhoon Mike in 1990 because the track was similar to Haiyan's track. The regional coupled model also simulated intensity changes of Typhoon Mike in 1990 realistically that underwent moderate intensification with the slow translation and large sea surface cooling.