Abstract
Longshore sediment transport presents an important problem at the shores along the Great Lakes. Direct field measurements were made on the parameters related to waves, beaches, longshore currents, and sediment transport. By using the field data from Lake Michigan, the longshore currents are found to be linearly related to the longshore momentum flux of incident waves at the breaker line, and also the longshore sediment immersed weight transport rate is found in terms of the longshore wave energy flux per unit length of beach.
Sign-in/Register to access full text options 
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.
