Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-OS Ocean Sciences & Ocean Environment

[A-OS14] Coastal physical processes associated with mixing, eddies, internal waves

Wed. May 29, 2019 3:30 PM - 5:00 PM 301A (3F)

convener:Eiji Masunaga(Ibaraki University), Taira Nagai(Graduate School of Science, The University of Tokyo), TSUTSUMI EISUKE(Atmosphere and Ocean Research Institute, The University of Tokyo), Chairperson:Eiji Masunaga, Taira Nagai

3:30 PM - 3:45 PM

[AOS14-07] Turbulent mixing and vertical nitrate flux in the Bungo Channel, Japan

*TSUTSUMI EISUKE1, Naoki Yoshie2, Takashi Mano3, Kanda Taisei3, Naoki Fujii4, Xinyu Guo2 (1.Research Institute for Applied Mechanics, Kyushu University, 2.Center for Marine Environmental Studies, Ehime Univeristy, 3.Graduate School for Science and Engineering, Ehime University, 4.Faculty of Agriculture, Saga Univerisity)

Keywords:turbulent mixing, vertical nitrate flux, internal tides

Turbulent mixing plays a key role in primary production in coastal seas through supplying nutrients to the euphotic zone from deeper layers and to the ocean from rivers. Understanding of turbulent dynamics in coastal seas is therefore essential for prediction, conservation and management of coastal ecosystems. Here, we studied turbulent mixing and the associated vertical nitrate transport in a tidally-energetic channel between the Kuroshio region and the Seto Inland Sea (Bungo Channel, Japan). Takeoka [1993] hypothesized that strong vertical mixing and the associated secondary circulation in the channel maintains primary production through supplying large amount of nutrients coming from the Kuroshio region. We conducted simultaneous measurements of turbulence and nitrate concentration along a section in the Bungo Channel using a microstructure turbulence profiler (TurboMAP-5, JFE Advantech) and optical nitrate sensor (SUNA-V2, Sea-Bird Scientific) on 27 August, 2017. We found nitrate-rich cold waters in the bottom of the southern part of the section, which coincide with a typical bottom intrusion from the Kuroshio region. Largest vertical eddy diffusivity of O(10-2) m2 s-1 and the associated upward nitrate flux of O(10) mmol m-2 day-1 were obtained at 20-30 m depth south of deep and narrow strait (Hoyo Strait). Also, subsurface maximum in chlorophyll fluorescence is observed just above the strong turbulence layer, possibly suggesting phytoplankton blooms in response to the high turbulent nitrate flux. The strong vertical turbulent diffusion was associated with density overturns and elevated vertical shear, indicating internal wave breaking. We hypothesis that internal tides generated in the Hoyo Strait is one of the key processes in enhancement of turbulent mixing and nutrient transport in the Bungo Channel.