日本地球惑星科学連合2016年大会

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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) 13:45 〜 15:15 302 (3F)

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)、座長:小玉 知央(独立行政法人海洋研究開発機構)

14:00 〜 14:15

[AAS02-02] Resolution dependence of diurnal cycle of tropical precipitation in a global high-resolution simulation

*八代 尚1梶川 義幸1宮本 佳明1吉田 龍二1山浦 剛1富田 浩文1 (1.国立研究開発法人 理化学研究所 計算科学研究機構)

キーワード:GCM, precipitation, high resolution simulation

We carried out the global high-resolution atmospheric simulations with five horizontal resolution from 14km to 0.87km. The Nonhydrostatic Icosahedral Atmospheric Model (NICAM; Satoh et al. 2014) was used for this study and both simulations and anarysis are conducted on the K computer. In the tropical region (15S-15N), the result shows clear resolution dependence of the diurnal precipitation cycle over the land. Relatively weak precipitation peak appeared at late night in the result of the coarse resolution. The peak becomes stronger and its time becomes faster with increasing the horizontal resolution. Theresolution dependence of temporal changes in the averaged environmental variables over the tropical land, such as CAPE, PBL height, cloud base height, and precipitable water, were analyzed. The result shows that the activation of the convections become earlier, especially in the simulations with grid spacing less than 2 km. This result suggests that the difference of convection activity around the noon at the different horizontal resolution affects timing of the peak of the daily precipitation.The early morning peak of tropical precipitation cycle over the ocean was also well reproduced, with lesser resolution dependence.