日本地球惑星科学連合2025年大会

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[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-CG36] 中緯度大気海洋相互作用

2025年5月26日(月) 10:45 〜 12:15 101 (幕張メッセ国際会議場)

コンビーナ: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(国立研究開発法人防災科学技術研究所)、桂 将太(東北大学大学院理学研究科地球物理学専攻)、座長:王 童(海洋研究開発機構)、桂 将太(東北大学大学院理学研究科地球物理学専攻)


11:15 〜 11:30

[ACG36-03] Intercomparison of eddy-resolving ocean reanalyses around Japan

*小守 信正1杉本 憲彦1久米田 健人1、森 日桜菜1宮本 佳明1広瀬 直毅2 (1.慶應義塾大学、2.九州大学)

キーワード:海洋再解析、西部北太平洋、黒潮、親潮、海洋前線、中規模渦

Ocean reanalysis datasets, created by assimilating observational data into numerical models, are becoming indispensable for studying past ocean variability. Increased computational power now enables us to conduct ocean reanalyses with a horizontal resolution of less than ten kilometers. In recent years, some operational centers have developed such "eddy-resolving" ocean reanalyses for regional or (quasi-)global oceans spanning several decades.
In this study, we compare three eddy-resolving ocean reanalyses—FORA-WNP30 (Usui et al., 2017), GLORYS12V1 (Lellouche et al., 2021), and BRAN2020 (Chamberlain et al., 2021)—for the western North Pacific around Japan. This region is characterized by oceanic fronts associated with the Kuroshio/Kuroshio Extension and Oyashio currents and contains detached mesoscale eddies. Our findings indicate that large-scale fields in the open ocean are highly similar due to the assimilation of observational data. However, significant discrepancies exist in mesoscale structures and in marginal seas.