日本地球惑星科学連合2021年大会

講演情報

[E] ポスター発表

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-AS01] 大規模な水蒸気場と組織化した雲システム

2021年6月4日(金) 17:15 〜 18:30 Ch.07

コンビーナ:横井 覚(海洋研究開発機構)、三浦 裕亮(国立大学法人 東京大学大学院 理学系研究科 地球惑星科学専攻)、濱田 篤(富山大学)、佐藤 正樹(東京大学大気海洋研究所)

17:15 〜 18:30

[AAS01-P01] Intraseasonal variability in the initialization of a seasonal prediction system simulated by a new convection scheme

★Invited Papers

*馬場 雄也1 (1.海洋研究開発機構)

キーワード:季節内振動、積雲対流スキーム、季節予測

Capturing interannual variability originating from coupled-mode phenomena such as El Nino Southern oscillation is important for seasonal prediction system, since the variability has great impact on seasonal variability. To obtain better prediction skill, recent prediction systems employ various assimilation techniques, but not only the assimilation but also improvements of physical parameterization is necessary, because the fidelity of the simulated variability significantly depends on model's physical performance. Large uncertainty is known to exist in the atmospheric component of the system, especially in the representation of clouds. Therefore, improving the parameterization of clouds is considered a key to improve model's performance, and also further improve the prediction skill. We implemented a new convection scheme in a seasonal prediction system (SINTEX-F2), and evaluated the impact of convection scheme in the initialization of the system which was done by SST nudging. In this study, we especially focused on the fidelity of the simulated intraseasonal variability (i.e., MJO) which can be influential to the formation of interannual variability. The first evaluation revealed that the model using different convection schemes simulated similar climatology and atmospheric response to interannual variability, with acceptable small climatological error diffrence. Qualitative analysises on MJO were conducted using the MJO diagnostics, and the analyses revealed that the new scheme outperformed the original scheme of the system. By using a composite analysis on the organized convection, it was found that the new scheme simulated moisture increase originating from shallow clouds in the advance of the organized convection, which indicated the original superiority of the new scheme (which has been already revealed in preceding studies) was obtained even in the present model. Statistical and quantitative evaluations were finally performed, indicating that the new scheme captured statistical behaviors of MJO better than the original scheme. In conclusion, the new convection scheme outperformed the original convection scheme of the system in terms of intraseasonal variability from various perspectives. The new scheme is therefore expected to improve the seasonal prediction skill, in particular, for the interannual variability which may be affected by the intraseasonal variability. The influence of the convection scheme in practical seasonal prediction should be studied and will be presented in our future study.