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- W2553529312 abstract "本研究では，気仙沼湾の狭水道部（大島瀬戸）において流速と水質の鉛直分布を15ヶ月間モニタリングし，流動とクロロフィル輸送の特徴を考察した．流速の残差流成分は+10～－40 mm/sであり，水深によらず10月から3月にかけて太平洋からの流入が強まり，5月から9月に流出が強まった．滞留時間は約11日となった．Chl-a輸送量は2014年3月～5月に太平洋からの流入が最大となり，6月～11月は流出，12月～2015年5月は流入が卓越した．T-Sダイアグラムから大島瀬戸の海底水の由来を判別し，平均流速とChl-a輸送量，沖合の海流状況を整理した結果，2014年春季に親潮由来の水塊が湾内に流入したと考えられ，親潮の南下接岸傾向によって大量の植物プランクトンが湾内に供給されると示唆された．" @default.
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- W2553529312 date "2016-01-01" @default.
- W2553529312 modified "2023-10-05" @default.
- W2553529312 title "HYDRODYNAMIC FLOW AND PHYTOPLANKTON TRANSPORTATION IN THE NARROW CHANNEL OF THE KESENNUMA BAY" @default.
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- W2553529312 doi "https://doi.org/10.2208/kaigan.72.i_1387" @default.
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