日本地球惑星科学連合2021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-OS 海洋科学・海洋環境

[A-OS10] 陸域海洋相互作用ー惑星スケールの物質輸送

2021年6月3日(木) 09:00 〜 10:30 Ch.11 (Zoom会場11)

コンビーナ:山敷 庸亮(京都大学大学院総合生存学館)、升本 順夫(東京大学大学院理学系研究科)、佐々木 貴教(京都大学 大学院理学研究科 宇宙物理学教室)、Behera Swadhin(Climate Variation Predictability and Applicability Research Group, Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001)、座長:升本 順夫(東京大学大学院理学系研究科)、Swadhin Behera(Climate Variation Predictability and Applicability Research Group, Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001)

09:15 〜 09:30

[AOS10-02] River-ocean interaction across a mega-delta

*木田 新一郎1、山崎 大2 (1.九州大学・応用力学研究所、2.東京大学・生産技術研究所)

キーワード:河川海洋相互作用、デルタ

The Ganges-Brahmaputra river is a major source of freshwater for the Bay of Bengal. River discharge occurs through the Ganges-Brahmaputra Delta, which consists of multiple river mouths. The seasonal cycle of this river discharge is observed with a minimum from late winter to early spring and a maximum from late summer to early fall. We investigated how the dynamics of this river discharge occurs near the river mouth based on a high-resolution numerical model that resolves the various channels of the Ganges-Brahmaputra Delta. The model simulates the basic seasonal cycle of the river discharge that is comparable to observations, with a river plume forming from the major river mouth and along the coast. We find that the river outflow through the main channel influences the surrounding narrow channels through the formation of this river plume by raising the sea level at the river mouth and reversing the direction of the flow. While the widths of these narrow rivers are narrow and less than the deformation radius, our model results suggest active river-ocean interaction occurring across the delta.