Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Hidekazu Yasuda"'
Autor:
Hidekazu Yasuda
Publikováno v:
Oceanography in Japan. 24:1-28
Publikováno v:
Oceanography in Japan. 19:263-282
Autor:
Hidekazu Yasuda
Publikováno v:
Journal of Oceanography. 65:455-476
Time-dependent wind drift currents in a basin with finite depth have been solved analytically in order to understand their fundamental behavior in coastal waters. The drift currents due to the land/sea breeze, as a typical example of time-dependent w
Autor:
Hidekazu Yasuda
Publikováno v:
PROCEEDINGS OF COASTAL ENGINEERING, JSCE. 54:356-360
Tidal currents were measured at the stationary station in the Suonda sound in late summer, 2005. The inertia current was obtained from the residual data which was produced by elimination of the main four tidal components, M2, S2, K1, and 01, from the
Autor:
Hidekazu Yasuda
Publikováno v:
Journal of Oceanography. 60:587-596
The fundamental nature of the mass flux due to the shear effect is examined analytically in a basin with steady and oscillatory currents to promote a better understanding of the mass transport process in coastal waters. The currents are given from so
Publikováno v:
Journal of Oceanography. 57:15-27
A hydrographic survey and a 25-hour stationary observation were carried out in the western part of Suo-Nada in the summer of 1998 to elucidate the formation mechanism of the oxygen-deficient water mass. A steep thermocline and halocline separated the
Autor:
Hidekazu Yasuda
Publikováno v:
Journal of Oceanography. 54:151-164
An analytical method for describing horizontal matter dispersion in shear currents is presented using a tensor expression from the point of view that matter dispersion due to the shear effect should be one of the principal mixing dilution processes.
Autor:
Hidekazu Yasuda
Publikováno v:
PROCEEDINGS OF HYDRAULIC ENGINEERING. 41:529-536
Matter dispersion due to the shear effect of currents is investigated theoretically as one of the mixing dilution processes. The shear is generated in the boundary layer as Stokes or Ekman layer which is given by motion equations. Dispersion of suspe
Autor:
Hidekazu Yasuda
Publikováno v:
Journal of Marine Research. 47:153-168
Autor:
Hidekazu Yasuda
Publikováno v:
Journal of the Oceanographical Society of Japan. 40:124-134
The horizontal circulations caused by the combined effect of the bottom oscillatory boundary layer (Stokes layer) and a sloping bed have been investigated both theoretically and experimentally. The generating mechanism is analogous to that for horizo