Abstract

Sandy beaches in estuaries and bays are distinct from open-coast beaches in that they are partially or fully sheltered from ocean waves. The sheltering increases the importance of other sources of wave energy such as infragravity waves that propagate into bays and estuaries with less dissipation than swell, combined with locally generated wind waves. Moreover, tidal translation and currents may become important and contribute to beach erosion and deposition. In this chapter, we review the importance of sandy beaches in estuaries and bays, and introduce the geological setting and oceanographic conditions that determine where they form and what they look like. We consider the variety of terminology that has been used to describe them (e.g. fetch-limited, low-energy or sheltered beaches) and discuss the relatively limited number of studies on their morphodynamics. We also include a case study from Botany Bay, Sydney, Australia. We conclude that sandy beaches in estuaries and bays should be recognised as a distinct class of beach (’bay and estuary beaches’, or BEBs) that has notable contrasts with open-ocean beaches that are dominated by ocean waves.

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.