日本地球惑星科学連合2016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23日(月) 09:00 〜 10:30 102 (1F)

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:滝川 雅之(独立行政法人海洋研究開発機構)

09:00 〜 09:15

[AAS02-13] Impacts of dense and frequent surface observations on a sudden severe rainstorm forecast: A case of an isolated convective system

*前島 康光1国井 勝2ルイス ファン3呉 宏堯4佐藤 香枝4三好 建正1 (1.理化学研究所 計算科学研究機構、2.気象研究所予報研究部、3.ブエノスアイレス大学、4.明星電気株式会社)

キーワード:Data assimilation, Sudden severe rainstorm forecast, An isolated convective system

To investigate the predictability at 1-km resolution for a sudden severe rainstorm event occurred on September 11, 2014 around Kobe city, we perform a series of data assimilation (DA) experiments using the Local Ensemble Transform Kalman Filter (LETKF) with the JMA-NHM (NHM-LETKF). In this event, a cumulonimbus generated suddenly near the Kobe city center around 0800 JST. It developed rapidly within 10-minutes, and brought heavy rainfalls over 50 mm h-1 from 0830 JST to 0930 JST, affecting people’s morning activities.
The control run (CTRL) was performed with only reflectivity and radial velocity data from the Phased Array Weather Radar (PAWR) in Osaka University. We installed the automated weather stations Meisei “POTEKA II” at 8 locations in Kobe city, and have been observing surface data every 30 seconds. We performed DA experiments with the additional temperature and relative humidity data from the surface stations. Since we found that the surface station data had significant biases, a bias correction method has been developed with the Kobe observatory data as the unbiased ground truth. Two DA experiments with the raw data (NOBC) and the bias corrected data (BC) have been performed.
CTRL showed strong echoes and surface rainfalls, although the rainfall intensity is smaller than the JMA analyzed precipitation based on the radar and gauge networks. NOBC showed a significant decrease in surface relative humidity because of the dry biases of the surface station data, and consequently, showed decreased surface rainfalls. By contrast, BC showed stronger rainfall intensity, better matching with the JMA analyzed precipitation. The results suggest that the dense and frequent surface DA have a potential to improve the forecast accuracy for sudden severe rainstorms.