日本地球惑星科学連合2022年大会

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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-OS22] 沿岸域の海洋循環と物質循環

2022年5月25日(水) 15:30 〜 17:00 展示場特設会場 (2) (幕張メッセ国際展示場)

コンビーナ:高橋 大介(東海大学)、コンビーナ:古市 尚基(水産研究・教育機構 水産技術研究所)、山口 一岩(香川大学)、コンビーナ:森本 昭彦(愛媛大学)、座長:高橋 大介(東海大学)、古市 尚基(水産研究・教育機構 水産技術研究所)、山口 一岩(香川大学)、森本 昭彦(愛媛大学)

16:00 〜 16:15

[AOS22-09] 女川湾における外洋水の流入とそれに伴う海洋構造の季節・経年変化

*高橋 大介1、金子 健司2 (1.東海大学、2.福山大学)

キーワード:季節変化、経年変化、海洋構造、外洋水の流入、女川湾

Seasonal and interannual variations in oceanographic conditions, such as water temperature and salinity, were investigated in Onagawa Bay on the Sanriku ria coast, which faces the Pacific Ocean, using hydrographic observations over the period of May 2012 to March 2019. Water temperature and salinity structure below the sea surface layer in the bay was seasonally affected by intrusions of oceanic water associated with the Oyashio water and the Tsugaru Warm Current water. Water mass distributions in the bay over the period of 2012 to 2015 had clear seasonality, characterized by the Oyashio water in the lower layer in spring, Tsugaru Warm Current water in the lower layer in fall and the entire water column in winter. This seasonality of water mass distributions was not distinct over the period of 2016 to 2019, that is, the Oyashio water did not appear in spring, but the Tsugaru Warn Current water frequently and intermittently intruded to the bay from spring to summer. Additionally, both water temperature and salinity in the bay tended to gradually increase over the entire period. During this time, warm water from the Kuroshio Extension stayed off the Sanriku ria coast and weaken intrusions of the Oyashio water to the bay. The results lead us to the conclusion that the interannual as well as seasonal variations of water temperature and salinity in Onagawa Bay are accompanied by the intrusions of oceanic water associated with the Oyashio water and Tsugaru Warm Current water.