日本地球惑星科学連合2014年大会

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インターナショナルセッション(口頭発表)

セッション記号 A (大気海洋・環境科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG04_1PM2] Hydroclimate in Asian monsoon region

2014年5月1日(木) 16:15 〜 18:00 413 (4F)

コンビーナ:*松本 淳(首都大学東京大学院都市環境科学研究科地理環境科学専攻)、里村 雄彦(京都大学大学院理学研究科地球惑星科学専攻)、樋口 篤志(千葉大学環境リモートセンシング研究センター)、鼎 信次郎(東京工業大学大学院情報理工学研究科)、高橋 洋(首都大学東京大学院都市環境科学研究科)、座長:高橋 洋(首都大学東京大学院都市環境科学研究科)、鼎 信次郎(東京工業大学大学院情報理工学研究科)

16:50 〜 17:05

[ACG04-09] 擬似温暖化手法を用いた地球温暖化に伴う日本周辺での台風特性の変化

*谷口 健司1細井 麻里2 (1.金沢大学 理工研究域 環境デザイン学系、2.金沢大学 自然科学研究科 環境デザイン学専攻)

キーワード:地球温暖化, 台風, 数値気象モデル, ダウンスケーリング

Results of global warming experiments indicate that an intensity of typhoon will be magnified in future climate. In this study, reproductive simulation of typhoons which approach to Japan are made. At the same time, pseudo global warming conditions are composed of a reanalysis product and multiple global warming experiments. Then, numerical simulations using the pseudo global warming conditions were conducted for each actual typhoon and variations of typhoons in future climate were investigated by comparing the reproductive simulation and the runs with pseudo global warming conditions. Results of a typhoon in summer showed significant variations in tracks. When a track deflects eastward, a typhoon goes over the ocean and its center pressure remarkably decreases. In addition, wind speed around the typhoon increases very much. Geopotential height in lower troposphere showed lower anomaly over the Pacific Ocean. Decreasing Pacific high is thought to be a cause of the change in typhoon tracks. In another typhoon in summer, although variations in tracks and center pressure were smaller, total precipitation in the typhoon increased in future. However, another typhoon in summer showed decreasing precipitation with small variation in tracks and center pressure. Results for another typhoon in autumn showed smaller variation in tracks and center pressures, and total precipitation increases in results of future climate. Such characteristics in future variations were found in other typhoons in autumn. On the other hand, hourly precipitations were not necessarily increased in future climate both in summer and autumn. These results indicate that extremely strong rainfall does not necessarily occur in short time, but modestly strong rainfall continues longer time. Even if no significant variation in center pressure, or intensity is similar to current climate, precipitation will increase in future climate.