大気水圏科学(A) | |||
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セッション小記号 | 大気科学・気象学・大気環境(AS) | ||
セッションID | A-AS09 | ||
タイトル | 和文 | Cloud-Resolving Model Simulations for Climate and Weather Studies | |
英文 | Cloud-Resolving Model Simulations for Climate and Weather Studies | ||
タイトル短縮名 | 和文 | Cloud-Resolving Model | |
英文 | Cloud-Resolving Model | ||
代表コンビーナ | 氏名 | 和文 | Toshihisa Matsui |
英文 | Toshihisa Matsui | ||
所属 | 和文 | NASA Goddard Space Flight Center | |
英文 | NASA Goddard Space Flight Center | ||
共同コンビーナ 1 | 氏名 | 和文 | 佐藤 正樹 |
英文 | Masaki Satoh | ||
所属 | 和文 | 東京大学大気海洋研究所 | |
英文 | Atmosphere and Ocean Research Institute, The University of Tokyo | ||
共同コンビーナ 2 | 氏名 | 和文 | Wei-Kuo Tao |
英文 | Wei-Kuo Tao | ||
所属 | 和文 | NASA Goddard Space Flight Center | |
英文 | NASA Goddard Space Flight Center | ||
発表言語 | E | ||
スコープ | 和文 | Cloud-resolving models (CRMs) employs nonhydrostatic dynamic core, explicit microphysics and radiation processes to provide physically-realistic simulations of cloud structures, optical properties, and latent heat release, without parameterizing deep convection in coarse-resolution weather and climate models. CRMs can be run at a few km down to sub-km of horizontal grid spacing depending on science application and focused cloud systems. Over the past few decades, CRMs have been utilized in a variety of weather and climate studies; such as 1) understanding cloud-precipitation processes and interactions with aerosols, surface, radiation, and lightning processes, 2) evaluating and developing microphysics and convection with various in-situ and remote sensing observations, and 3) addressing climate issues to develop or replace convective-cloud parametrizations for global or regional atmospheric models. The goal of this session is to showcase the current efforts for these studies in the atmospheric community. | |
英文 | Cloud-resolving models (CRMs) employs nonhydrostatic dynamic core, explicit microphysics and radiation processes to provide physically-realistic simulations of cloud structures, optical properties, and latent heat release, without parameterizing deep convection in coarse-resolution weather and climate models. CRMs can be run at a few km down to sub-km of horizontal grid spacing depending on science application and focused cloud systems. Over the past few decades, CRMs have been utilized in a variety of weather and climate studies; such as 1) understanding cloud-precipitation processes and interactions with aerosols, surface, radiation, and lightning processes, 2) evaluating and developing microphysics and convection with various in-situ and remote sensing observations, and 3) addressing climate issues to develop or replace convective-cloud parametrizations for global or regional atmospheric models. The goal of this session is to showcase the current efforts for these studies in the atmospheric community. | ||
発表方法 | 口頭および(または)ポスターセッション |