JpGU-AGU Joint Meeting 2017

講演情報

[EE] 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-AS12] [EE] 高性能スーパーコンピュータを用いた最新の大気科学

2017年5月20日(土) 10:45 〜 12:15 101 (国際会議場 1F)

コンビーナ: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)、小玉 知央(独立行政法人海洋研究開発機構)、滝川 雅之(独立行政法人海洋研究開発機構)、座長:小玉 知央 (国立研究開発法人 海洋研究開発機構)、座長:滝川 雅之(国立研究開発法人 海洋研究開発機構、国立研究開発法人 海洋研究開発機構)

11:15 〜 11:30

[AAS12-09] Status and outlook of a high-resolution climate simulation using NICAM toward CMIP6 HighResMIP

*小玉 知央1大野 知紀2野田 暁1八代 尚3山田 洋平1中野 満寿男1清木 達也1那須野 智江1Chen Ying-Wen1宮川 知己2佐藤 正樹1,2杉 正人4 (1.独立行政法人海洋研究開発機構、2.東京大学大気海洋研究所、3.理化学研究所計算科学研究機構、4.気象研究所)

キーワード:high-resolution climate simulation, CMIP6 HighResMIP, sensitivity experiments, climate bias, tropical cyclone

Climate simulation using a global model with a mesh size of O (10 km) becomes more common than ever thanks to the rapid advancement in high performance computer. Such a fine-mesh global climate simulation represents atmospheric multi-scale phenomena ranging from large-scale circulation to meso-scale features associated with convection, front, severe rainfall, atmospheric gravity wave and so on in a seamless manner. Tropical cyclone is an excellent example of multi-scale interactions. Its generation, development and track are strongly influenced by larger-scale mean state and disturbances. To this end, we have performed a first-ever AMIP-type climate simulation using a 14-km mesh non-hydrostatic global atmospheric model, NICAM, without convection scheme and shown a good performance in the simulated climatology of tropical cyclone as well as a wide variety of atmospheric phenomena including tropical wave and precipitation (Kodama et al. 2015). We have also found some significant climate biases which might hinder a reliable projection of future climate.
Here we will present a status and an outlook of a high-resolution climate simulation using the latest version of NICAM. A series of new climate simulations under a framework of CMIP6 HighResMIP (High Resolution Model Intercomparison Project) and DynVAR (Dynamics and Variability Model Intercomparison Project) are planned. An impact of the horizontal resolution on weather and climate phenomena will be investigated by preforming the model with a mesh sizes of 14, 28 and 56 km. Physics schemes including cloud microphysics, gravity wave drag, aerosol and land model are under updating and/or tuning to improve the simulated climatology. As an example, a better performance in the simulated top-of-the-atmosphere radiation balances is found in the latest version of NICAM with a new cloud microphysics scheme, which was validated by a satellite measurement with a focus on cloud-precipitation processes (Roh and Satoh 2014). In addition, some fresh results from a series of short-term sensitivity experiments will be presented and discussed in this talk.