日本地球惑星科学連合2016年大会

講演情報

インターナショナルセッション(口頭発表)

セッション記号 A (大気水圏科学) » A-CG 大気水圏科学複合領域・一般

[A-CG08] Continental-Oceanic Mutual Interaction: Global-scale Material Circulation through River Runoff

2016年5月23日(月) 09:00 〜 10:30 A04 (アパホテル&リゾート 東京ベイ幕張)

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)、宮澤 泰正(独立行政法人海洋研究開発機構)、Behera Swadhin(Climate Variation Predictability and Applicability Research Group, Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001)、山形 俊男(海洋研究開発機構 アプリケーションラボ)、寶 馨(京都大学防災研究所)、座長:升本 順夫(東京大学大学院理学系研究科)、Behera Swadhin(Japan Agency for Marine-Earth Science and Technology)、山形 俊男(海洋研究開発機構 アプリケーションラボ)

09:45 〜 10:00

[ACG08-04] Development of an ocean-river-surface runoff seamless model

*木田 新一郎1 (1.Japan Agency for Marine-Earth Science and Technology)

キーワード:surface runoff, river discharge, oceanic model

The ocean receives significant amount of freshwater through river discharges. One of the challenges of regional-scale numerical ocean models is to capture this input of freshwater that often occurs spontaneously. Weather events are not well captured by monthly data sets that are publically available. The boundary between river water and oceanic water masses are also difficult to capture with a lateral boundary condition that is physically fixed in space. In order to simulate the movement of freshwater cycle from land to the ocean, we have developed an ocean-river-surface runoff seamless model based on an oceanic isopycnal model. This approach enables simulations of river discharge events based on precipitation data, which is more publically available in space and time, compared to river discharge data. The movement of water based is also solved with a same dynamical core. We previously demonstrated the capability of this new approach through validation of Abukuma river discharge event during a typhoon. We now extend this model to solve the rivers of main Japanese islands for various other rivers. Preliminary results show promising results, with multiple freshwater plumes forming at various river mouths of Japan, small to large, as the center of the typhoon moves from south to north.