Japan Geoscience Union Meeting 2018

Presentation information

[EE] Oral

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

[A-OS11] What we have learned about ocean mixing in the last decade

Mon. May 21, 2018 1:45 PM - 3:15 PM 105 (1F International Conference Hall, Makuhari Messe)

convener:Toshiyuki Hibiya(Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo), Louis St Laurent (Woods Hole Oceanographic Institution), Ren-Chieh Lien(None, 共同), Robin Ann Robertson (China-ASEAN College of Marine Science Xiamen University Malaysia), Chairperson:Hibiya Toshiyuki(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo)

3:00 PM - 3:15 PM

[AOS11-18] The Mixing of Cold Water Upwelled in the Upper Ocean Turbulent Boundary Layer by an Artificial System

*Alexander Soloviev1, Cayla Dean1 (1.Nova Southeastern University)

Keywords:upwelling, stratification, shear, mixing

Artificial upwelling driven by surface waves can provide significant societal benefits ranging from maricultural farming to modification of extreme local climates. One of the first upwelling deices using the energy of surface waves (wave-inertia pump) was developed and tested on the Black Sea by Vershinsky et al. (1987). (This design is believed to be the most efficient artificial upwelling system even now.) The cold water upwelled by a wave-inertia pump is of a higher density and therefore thinks back down in the form of a convective jet, which resembles the convective jet in the atmospheric turbulent boundary layer. The plunging jet triggers Kelvin-Helmholtz instability in the shear layer at the bottom of the mixed layer and in the thermocline, thereby increasing vertical mixing in the thermocline and entrainment of cold water to the mixed layer. The process has been simulated using ANSYS Fluent computational fluid dynamics software. The large eddy simulation indicates that there is an increase of the mixing efficiency due to developing coherent structures in the form of of Kelvin-Helmholtz billows. We have considered the potential application of the artificial upwelling system for reduction of hurricane intensity in coastal areas, before the hurricane landing, and mitigation of the arid climate in the Levant. The ocean heat content (OHC) is the "fuel" for hurricanes. The surface layer mixing with the upwelled cold water produced by wave-inertia pumps reduces the OHC accessible to hurricanes. At the same time, the results of the numerical simulation indicate that some additional heat is accumulated below the thermocline. Long term observations have shown a correlation between the heat content accumulated during summer off the coastline of Haifa and precipitation in Jerusalem in winter. By increasing upper ocean mixing, an artificial upwelling system on the Israel coast of the Mediterranean Sea is expected to increase precipitation in the Levant during wintertime and reduce air-temperature in summer. Computer simulation can help us better understand the feasibility of these geoengineering approaches and their environmental consequences.

Reference: Vershinsky, N.V., Pshenichnyy, B.P., and Soloviev , A.V., 1987: Artificial upwelling using the energy of surface waves. Oceanology 27(3), 400-402.