Abstract

Surface and bottom currents in the surf zone were measured at 15 equally spaced points along two straight beaches with approximately parallel bottom contours. The measurements showed that offshore currents predominate over onshore currents at the bottom, while at the surface there is a slight predominance in the onshore direction. With regard to the longshore component, it was found that surface and bottom currents have a similar velocity distribution. The variability of the longshore component as measured by its standard deviation is equal to or larger than the mean longshore velocity. This wide variation in longshore currents indicates the impracticability of estimating the mean velocity from a single observation of longshore current. It was found that the momentum approach to the prediction of longshore currents by Putnam, Munk and Traylor (1949) leads to useful forecasts provided the beach friction coefficient k is permitted to vary with the longshore velocity, V. The indicated relation is k~v^(-3/2).

Highlights

  • A series of longshore current measurements was made in 1949 and 1950 along two straight beaches in the San Diego area

  • The terminology and general principles of the circulation resulting from wave action in and near the surf zone was discussed in a previous paper (Shepard and Inman, 1951)

  • Two straight beaches with relatively parallel bottom contours were selected for study, Torrey Pines beach north of La Jolla and Pacific Beach to the south of La Jolla (Pig. 1)

Read more

Summary

Introduction

A series of longshore current measurements was made in 1949 and 1950 along two straight beaches in the San Diego area.

Results
Conclusion
Full Text
Paper version not known

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

Disclaimer: 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.