日本地球惑星科学連合2023年大会

講演情報

[E] オンラインポスター発表

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-CG30] 中緯度大気海洋相互作用

2023年5月22日(月) 13:45 〜 15:15 オンラインポスターZoom会場 (2) (オンラインポスター)

コンビーナ:関澤 偲温(東京大学先端科学技術研究センター)、桂 将太(東京大学大気海洋研究所)、安藤 雄太(九州大学)、木戸 晶一郎(海洋開発研究機構 付加価値創生部門 アプリケーションラボ)


現地ポスター発表開催日時 (2023/5/21 17:15-18:45)

13:45 〜 15:15

[ACG30-P14] Large-scale atmospheric response to warm SST anomalies in the North Pacific in the 2021-22 winter

*西井 和晃1田口 文明2中村 尚3 (1.三重大学大学院生物資源学研究科、2.富山大学都市デザイン学部、3.東京大学先端科学技術研究センター)

キーワード:AGCM resolution、PDO、blocking、stratospheric vortex

Sea surface temperatures (SST) in the North Pacific were extremely warm in the 2021-22 winter associated with the negative phase of the Pacific Decadal Oscillation (PDO). We investigate the large-scale atmospheric responses to the warm SST anomalies through ensemble time-slice experiments of an atmospheric general circulation model (AGCM) with two different horizontal resolution settings: 100 km and 50 km. In both the 100-km and 50-km experiments, anticyclonic responses in the winter-mean 500-hPa geopotential height fields are found over the North Pacific. The anticyclonic response is stronger in the 50-km AGCM, and its center is located slightly to the west of that obtained in the 100-km AGCM. Blocking frequency over the North Pacific in the 50-km AGCM is significantly increased under the influence of the warm SST anomalies, which may cool the lower stratosphere in the Arctic through suppressing upward planetary-wave propagation from the troposphere. Such increased blocking and cooling in the polar stratosphere are not observed in the response in the 100-km AGCM, suggesting the need for a high-resolution model to obtain a realistic blocking response to midlatitude SST anomalies.