Three-dimensional modeling of tidal circulation and mixing over the Java Sea |
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| Authors: | Alan F Koropitan Motoyoshi Ikeda |
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| Institution: | (1) Graduate School of Environmental Science, Hokkaido University, Kita-ku, Sapporo 060-0810, Japan;(2) Department of Marine Science and Technology, Bogor Agricultural University (IPB), Kampus IPB Darmaga, Bogor, 16680, Indonesia |
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| Abstract: | A combination of a three-dimensional hydrodynamic model and in-situ measurements provides the structures of barotropic tides,
tidal circulation and their relationship with turbulent mixing in the Java Sea, which allow us to understand the impact of
the tides on material distribution. The model retains high horizontal and vertical resolutions and is forced by the boundary
conditions taken from a global model. The measurements are composed of the sea level at coastal stations and currents at moorings
embedded in Seawatch buoys, in addition to hydrographic data. The simulated tidal elevations are in good agreement with the
data for the K1 and M2 constituents. The K1 tide clearly shows the lowest mode resonance in the Java Sea with intensification around the nodal point in the central region.
The M2 tide is secondary and propagates westward from the eastern open boundary, along with a counterclockwise amphidromic point
in the western part. The K1 tide produces a major component of tidal energy, which flows westward and dissipates through the node region near the Karimata
Strait. Meanwhile, the M2 tide dissipates in the entire Java Sea. However, the residual currents are mainly induced by the M2 tide, which flows westward following the M2 tidal wave propagation. The tidal mixing is mainly caused by K1 tide which peaks at the central region and is consistent with the uniform temperature and salinity along the vertical dimension.
This mixing is expected to play an important role in the vertical exchange of nutrients and control of biological productivity. |
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| Keywords: | Hydrodynamic model barotropic tides Java Sea resonance tidal energy residual currents tidal mixing |
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