日本地球惑星科学連合2018年大会

講演情報

[JJ] ポスター発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS15] 海洋と大気の波動・渦・循環力学

2018年5月20日(日) 15:30 〜 17:00 ポスター会場 (幕張メッセ国際展示場 7ホール)

コンビーナ:古恵 亮(APL/JAMSTEC)、田中 祐希(東京大学大学院理学系研究科)、久木 幸治(琉球大学、共同)、杉本 憲彦(慶應義塾大学 法学部 日吉物理学教室)

[AOS15-P06] 渦解像OGCMを用いた北太平洋亜寒帯の中暖中冷構造再考

*中野 英之1辻野 博之1坂本 圭1浦川 昇吾1豊田 隆寛1山中 吾郎1 (1.気象研究所)

キーワード:海洋大循環モデル、フロント、温度逆転

The formation and distribution of the mesothermal and dichothermal structures (temperature inversions) in the North Pacific are investigated using an eddying (1/10 x 1/10) Pacific OGCM. The distribution of the modeled inversions are closely related to the strong currents in the northern North Pacific, indicating that lateral advection is essential for its distribution and temporal variability. The modeled mesothermal structures are found more than 90% of the year in the Subarctic gyre west of the dateline and along the Subarctic Current (SAC). Its southern boundary is quite distinct between the dateline and the Gulf of Alaska. Its northern and eastern boundary is are somewhat unclear partly due to the presence of strong mesoscale rings in the Gulf of Alaska and along the Alaskan Stream. In winter and spring, they are found along the current associated with the Subarctic Boundary (SAB-C) and Alaskan Stream. The distribution of the modeled dichothermal structure is similar to that of the mesothermal structure, but the region where the dichothermal structure is found more than 90% is only limited along the SAC and shows a large inter-annual variability. In these areas the dichothermal structures are created upstream and advected downstream below the seasonal thermocline. These findings in the model is consistent with that found in the WOA13.