日本地球惑星科学連合2024年大会

講演情報

[E] 口頭発表

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-CG32] 中緯度大気海洋相互作用

2024年5月26日(日) 13:45 〜 15:15 201B (幕張メッセ国際会議場)

コンビーナ:桂 将太(東北大学大学院理学研究科地球物理学専攻)、安藤 雄太(九州大学大学院理学研究院)、王 童(海洋研究開発機構)、田村 健太(北海道大学大学院地球環境科学研究院)、座長:桂 将太(東京大学大気海洋研究所)、王 童(海洋研究開発機構)


14:00 〜 14:15

[ACG32-11] Oceanic Reemergence Memory Links Atlantic and Pacific Multidecadal Variability

★Invited Papers

*BAOLAN WU1、LISAN YU2、XIAOPEI LIN3、JIANPING GAN1、BO QIU4、LIXIAO XU3 (1.HKUST、2.WHOI、3.OUC、4.U Hawaii)

キーワード:mode water, multidecadal variability, Pacific , Reemergence, Oceanic memory

Understanding how the ocean provides the memory needed for maintaining decadal to multidecadal variability is key to climate prediction. An important question is what process in the ocean could provide the observed significant time-lag between the Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO). Here we show that the Pacific Ocean could store climate anomalies within the subtropical recirculation gyre for a decadal duration, providing a “seeding” link between the AMO and PDO. The AMO-induced multidecadal temperature anomalies in the Subtropical Northwestern Pacific Ocean are subducted into the thermocline and sequestered in the North Pacific subtropical mode water. These temperature anomalies carried by the mode water would propagate southwestward along the recirculation gyre pathway to eventually re-join the Kuroshio one decade later. Once reemerged in the isopycnal outcropping area of the Kuroshio-Oyashio Extension region, the anomalies that carry the memory of the previous decade may engage with local air-sea feedback to trigger the PDO. Thus, the AMO provides important memory for prediction of decadal climate and ecosystem variability in the Pacific Ocean.