z-logo
open-access-imgOpen Access
Lagrangian Solution for an Irrotational Progressive Water Wave Propagating on a Uniform Current
Author(s) -
Yang-Yih Chen,
Hsuan-Shan Chen,
Chuyu Lin,
Meng-Syue Li
Publication year - 2013
Publication title -
journal of atmospheric and oceanic technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.774
H-Index - 124
eISSN - 1520-0426
pISSN - 0739-0572
DOI - 10.1175/jtech-d-12-00171.1
Subject(s) - physics , mechanics , particle velocity , trajectory , particle (ecology) , magnetosphere particle motion , classical mechanics , wavelength , conservative vector field , optics , geology , oceanography , quantum mechanics , astronomy , magnetic field , compressibility
Experiments are conducted to measure the motion properties of water particle for the progressive water wave propagation in the presence of following and adverse uniform currents. The experimental data are used to validate the fifth-order Lagrangian solution from Chen and Chen. The experimental results show that the measured data of the particle motion properties such as the b line (denoted as the line connecting the positions of consecutive particles of the same b label), the particle velocity, the particle transport velocity (drift velocity), the particle trajectory, the particle motion period, and the Lagrangian mean level are in close agreement with those of the fifth-order Lagrangian solution. The study also shows that the particle label could adopt the position coordinates of the particle as if it were in still water. The motion of the b line oscillates like wave motion: its wavelength is equal to the progressive wavelength and its wave velocity obeys the Doppler effect so the sum of the velocities of the progressive wave and current, the particle motion period, the Lagrangian mean level, and the particle transport velocity less current velocity are the same as for the case of pure progressive waves. For following currents, the shape of particle trajectory depends on the horizontal particle velocity at the trajectory trough. For adverse currents, the shape of particle trajectory depends on the horizontal particle velocity at the trajectory crest. For a description of the flow motion, the Lagrangian solution could be more effective and precise than the Eulerian solution.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here