日本地球惑星科学連合2024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-CG 大気海洋・環境科学複合領域・一般

[A-CG31] Climate Variability and Predictability on Subseasonal to Centennial Timescales

2024年5月27日(月) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:Murakami Hiroyuki(Geophysical Fluid Dynamics Laboratory/University Corporation for Atmospheric Research)、森岡 優志(海洋研究開発機構)、Kataoka TakahitoYang Xiaosong(NOAA Geophysical Fluid Dynamics Laboratory)

17:15 〜 18:45

[ACG31-P01] Multi-year predictive skill of the wintertime heavy rainfall potentials in western Japan

*望月 崇1 (1.九州大学大学院理学研究院)

キーワード:近未来予測、海盆間相互作用、極端降水、顕著現象、大規模アンサンブルシミュレーション

Statistical changes in extreme weather and climate events have attracted much attention as potential sources of natural disasters. Numerical experiments to obtain huge ensembles of multiyear predictions with initialization using a high-resolution model represent a direct approach but a difficult solution for the computational resources available currently. Here, we validated the multiyear predictive skills of wintertime heavy rainfall potential in western Japan, by combining initialized decadal hindcasts of the global climate model and large ensemble simulations from a high-resolution global atmospheric model. By analyzing a set of initialized hindcasts, we identified one of the major predictive components of sea surface temperature (SST) variability beyond interannual timescales as the so-called trans-basin variability. A set of 100 ensemble simulations using a high-resolution atmospheric model show a significantly large signal-to-noise ratio for the wintertime heavy rainfall potential in western Japan, which is closely related to the trans-basin variability. When the SST around the maritime continent is higher, the anomalously low pressure in the northwestern Pacific enhances low-level cold air transport due to the winter monsoon. Consequently, the resultant weaker baroclinicity in the lower atmosphere reduces storm activity and wintertime heavy rainfall potential in western Japan.