For the Instructor
These student materials complement the Coastal Processes, Hazards and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.Wave, Mixed Energy, and Tide Dominated Hydrographic Regimes
Our understanding of waves and tides now sets the stage for a more thorough understanding of how they interact to shape a coastal zone. In the context of hydrographic regime, there are two fundamental things that must be considered: the wave and tidal energy of a coast.
- Wave energy (E) is a function of wave height (H) with the energy (E) of a wave approximately equal to the square of the wave height (H2).
- Tidal energy can be equated with tidal range, because it is the rise and fall of the tides that produce tidal currents. Tidal range (TR) is the vertical difference between high and low tides, which are commonly categorized into three ranges: Microtidal TR < 2.0 m, Mesotidal 2.0 m < TR < 4.0 m, and Macrotidal TR > 4.0 m
The relative dominance of wave versus tidal energy dictates coastal morphology and three general regimes exist along depositional coasts:
- Wave Dominated Coasts
- Mixed Energy Coasts
- Tide-dominated Coasts