The wave base, in physical oceanography, is the maximum depth at which a water wave's passage causes significant water motion. For water depths deeper than the wave base, bottom sediments and the seafloor are no longer stirred by the wave motion above.
In seawater, the water particles are moved in a circular orbital motion when a wave passes. The radius of the circle of motion for any given water molecule decreases exponentially with increasing depth. The wave base, which is the depth of influence of a water wave, is about half the wavelength.
At depths greater than half the wavelength, the water motion is less than 4% of its value at the water surface and may be neglected.
For example, in a pool of water 1 metre (3.3 ft) deep, a wave with a 3 metres (9.8 ft) wavelength would be moving the water at the bottom. In the same pool, a wave with a wavelength of 0.5 metres (1.6 ft) would not be able to cause water movement on the bottom.
There are typically two wave bases, the fair weather wave base (FWWB) and the storm wave base (SWB).
The storm wave base refers to the depths beneath storm-driven waves and can be much deeper. The portion of the seafloor that is only agitated by storm-driven wave action is known as the Lower shoreface.
Note that another classification exists, which considers that the zone affected by both fair weather and storm waves is to be defined as shoreface, whereas Upper offshore is the name given to the zone only affected by storm waves and Lower offshore a zone not disturbed by any surface wave. (e.g. )
Types Of Wave Bases
fair weather base: it is a sea depth of 5 to 15m below sea level where the sea bed is unaffected by the action of waves in the calm wave conditions.
- Upper shoreface — above wave base
- Lower shoreface — below wave base
- Airy wave theory
- Dispersion (water waves)
- Waves and shallow water
- R. G. Dean & R. A. Dalrymple (1991). Water wave mechanics for engineers and scientists. Advanced Series on Ocean Engineering. 2. World Scientific, Singapore. ISBN 978-981-02-0420-4.
- At a depth of half the wave length, the amplitude of the water particle motion by the waves has been reduced to e−π ≈ 0.04 times it value at the water surface.
- Bayetgoll et al., 2015, Ichnology and sedimentology of a shallow marine Upper Cretaceous depositional system (Neyzar Formation, Kopet-Dagh, Iran): Palaeoceanographic influence on ichnodiversity, Cretaceous Research, 56, 628-646