*吉江 直樹1、大城 一輝1、加部 晏諒1、林 由真1、小針 統2、堤 英輔3、長谷川 大介4、石坂 丞二5 (1.愛媛大学沿岸環境科学研究センター、2.鹿児島大学水産学部、3.東京大学大気海洋研究所、4.水産研究教育機構東北区水産研究所、5.名古屋大学宇宙地球環境研究所)
セッション情報
[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-OS24] Exploring new frontiers of oceanic mixing research in the next decade
コンビーナ:日比谷 紀之(東京大学大学院理学系研究科地球惑星科学専攻)、安田 一郎(東京大学大気海洋研究所)、Lakshmi Kantha(Aerospace Engineering Sciences, University of Colorado, Boulder, Colorado, USA)
Mixing plays many important roles in the global ocean through a variety of different processes. In the upper ocean, mixing affects the sea surface temperature and hence air-sea interactions, which in turn influence the state of the atmosphere on a variety of time scales. Mixing in the deep ocean maintains the abyssal stratification of the world's oceans and influences the global overturning circulation, which in turn affects long-term climate. Ocean mixing modulates the transport and dispersal of dissolved and suspended materials, including pollutants, plankton and fish larvae. It also plays an important role in the oceanic food chain in so far as primary productivity, which occurs predominantly in the euphotic zone, is affected by nutrient uptake from the deep associated with ocean mixing.
Microstructure profilers are being increasingly and routinely used to measure turbulence in the oceans, including the deep. Mixing models with more inclusive physics are being developed. Increasing computer power is making it possible to include sophisticated mixing models in global circulation models. As such, it is time to take stock of where we stand at present and explore the frontiers of mixing research over the next decade to advance our knowledge and utilize it for societal benefit.
This session encompasses a wide variety of aspects of mixing within the water column from the surface to the seabed, as well as the impact of mixing on key physical, biological, and chemical processes, such as those mentioned above, with special attention to new findings obtained through improvements in oceanographic instrumentation, mixing models and the use of supercomputers. Observational, theoretical, experimental, and numerical approaches are all welcome. In this session, we particularly encourage discussion that can confirm how far our understanding of related topics has advanced and help define the new frontiers of ocean mixing research to be tackled in the next decade.
*上野 洋路1、土橋 稜2、岡田 友希2、田中 雄大3、西岡 純4、平譯 享1、大木 淳之1、伊藤 幸彦5、笹井 義一6、佐々木 英治6、安田 一郎5 (1.北海道大学 大学院水産科学研究院、2.北海道大学 大学院水産科学院、3.水産研究・教育機構 東北区水産研究所、4.北海道大学 低温科学研究所、5.東京大学 大気海洋研究所、6.海洋研究開発機構)
*西岡 純1,2、小畑 元3、平譯 享2,4、山下 洋平5、小川 浩史3、安田 一郎3 (1.北海道大学低温科学研究所、2.北海道大学北極域研究センター、3.東京大学大気海洋研究所、4.北海道大学大学院水産科学研究院、5.北海道大学大学院地球環境科学研究院)
講演取消