@article{oai:ir.kagoshima-u.ac.jp:00007827,
 author = {KIKUKAWA, Hiroyuki},
 journal = {鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University},
 month = {2016-10-28},
 note = {The tidal residual flow in Kagoshima bay is evaluated by employing the two-dimensional
explicit weighed residual method for space, which conserves the water mass, and the two-step
Lax-Wendroff method for time differentiation. Water surface elevation is given at the open
boundary and the non-slip boundary condition is adopted at the coast. In order to obtain
stable results, calculation is performed over five period.
The estimated tidal residual flow shows that there exists a large anti-clockwise vortex at
the center of the bay and that the water mass inflows from the east side and outflows from
the west side of the mouth of the bay. In spite of the roughness of the division of the bay,
the above two features of the results are similar to the observational results so far
performed.},
 pages = {29--48},
 title = {Numerical Calculation of Tide in Kagoshima Bay : Part 2. Two-dimensional Explicit Weighted Residual Method},
 volume = {32},
 year = {}
}