Abstract
The author observed a tidal current using his current meter [1]and two others of different kinds simultaneously. He explained that the observed velocity fluctuation with the period of 1.5 hours was caused by the instantaneous penetration of the waters broken from the disturbance, and the time variation of velocity was due to the effect of vertical eddy viscosity and the change of the surface slope with time Further. he analysed the shorter period disturbance and found that its eddy diffusion coefficient K∼269 c. g. s, its mean length of edddy l∼124 cm.
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 callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
