Abstract
In this paper, we investigate the mean velocities in an irrotational periodic geophysical traveling surface wave, which propagates in equatorial oceanic regions. Employing the harmonic and complex analysis in combination with exploiting some of the physical structures of the problem, we prove that the horizontal mean velocity is less than the depth-averaged velocity in the frame of reference in which the wave is stationary.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
