日本地球惑星科学連合2025年大会

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[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-CG40] 大気・海洋観測の気候・海洋予測へのインパクト評価

2025年5月27日(火) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:藤井 陽介(気象庁気象研究所)、木戸 晶一郎(海洋研究開発機構 付加価値情報創生部門 アプリケーションラボ)、Tseng Yu-heng(Institute of Oceanography, National Taiwan University)、Xie Jiping(Nansen Environmental and Remote Sensing Center, Norway)


17:15 〜 19:15

[ACG40-P09] High-Resolution Regional Ocean Modeling of the East/Japan Sea: Resolving Submesoscale Dynamics and Wind Forcing Effects

*HaeIn Kim1、Young Ho Kim1、Eun Young Lee2、Dong Eun Lee2 (1.Pukyong National University、2.Chungnam National University)

キーワード:Regional Ocean Modeling , MOM6, submesoscale eddies, hybrid coordinate

The East/Japan Sea (EJS) is a semi-enclosed sea located in the mid-latitude East Asian Sea that exhibits many characteristics of large-scale ocean systems. Cold waters from the Okhotsk Sea in the north and warm waters from the East China Sea in the south converge to form a zonally oriented polar front approximately 39–40°N. Along this front, submesoscale eddies emerge from the interplay of mesoscale eddies, topography, and local oceanographic conditions. These eddies play a key role in enhancing turbulent mixing, facilitating the upward transport of nutrients, and promoting phytoplankton productivity, even though large areas of the EJS remain underobserved, leaving gaps in understanding its complex dynamics.
This study presents the establishment and evaluation of a high-resolution (1/48°) regional ocean model for the EJS using GFDL MOM6 (Modular Ocean Model Version 6). The model is configured on an Arakawa C-grid with a spatial resolution of approximately 2 km and employs a hybrid vertical coordinate system that combines z* and isopycnal coordinates with 75 layers. The initial and open boundary conditions are taken from high-resolution (1/24°) Northwest Pacific Ocean reanalysis (KOOS-OPEM), which effectively reproduces the key features of the EJS.
We investigated the sensitivity of the East Korea Warm Current (EKWC), a western boundary current, to wind forcing. We examined the separation latitude of the EKWC under different wind forcing datasets, including the ERA5 dataset from ECMWF and the UM model from the Korea Meteorological Administration. Furthermore, to assess the representation of submesoscale eddies, the kinetic energy spectrum and systematic evaluation will be displayed.