Glossary
- Beaufort Wind Force Scale
- A thirteen-step scale of wind speeds (Force 0 to Force 12) based on observations of the effects at sea and on land.
- Coriolis effect
- The apparent tangential acceleration of an object moving towards or away from an axis around which it is moving.
- Reynolds number
- A dimensionless number that indicates the relative importance of inertial and viscous forces and also the likelihood of turbulent flow. Reynolds numbers are frequently used to compare flow patterns.
- amphidromic point
- A point with no tidal rise or fall. Also called a tidal node.
- amphidromic system
- A system (e.g. the North Sea or the Sound of Jura) containing an amphidromic point.
- amplitude
- The maximum extent of a vibration, oscillation or periodic function, measured from the position of equilibrium or centre line. The amplitude of a sinusoidal curve is half the difference between the maximum and minimum values of the curve.
- anticyclones
- The large-scale atmospheric rotation around an area of high pressure. Anticyclonic rotation is clockwise in the northern hemisphere and anti-clockwise south of the equator.
- atmospheric boundary layer
- The region of the atmosphere, up to about 1000 m above ground level, in which interaction with the ground significantly affects wind speed and direction.
- break
- A water wave breaks when it changes from approximately sinusoidal in shape to hooked prior to the crest collapsing. Waves may break as a result of wind action, moving into shallower water or a combination of both.
- crest
- The top of a water wave.
- currents
- Bulk flow in the atmosphere or oceans.
- cyclones
- The large-scale atmospheric rotation around an area of low pressure. Cyclonic rotation is anti-clockwise in the northern hemisphere and clockwise south of the equator. A cyclone is also the name for a hurricane when south of the equator.
- depression
- An area of atmospheric low pressure. Also called a low.
- design wave
- The likely worst-case wave height, used as a factor in the design of structures that interact with the sea.
- design wind speed
- The likely highest wind speed, used as a factor in the design of structures that interact with the atmosphere.
- double tides
- Two high tides in close succession with a small drop in between (or two low tides in close succession with a small rise in between).
- drag coefficient
- A non-dimensional form of drag: the drag force produced as a fraction of the product of stagnation pressure and a characteristic area. See also lift coefficient.
- ebb
- The receding or downward-going tide.
- fetch
- The distance over which wind can build up waves at sea.
- flood
- The approaching or upward-going tide.
- geostrophic winds
- Winds above the atmospheric boundary layer, driven by pressure gradients and Coriolis forces. Also called gradient winds.
- gradient winds
- See geostrophic winds.
- ground level to reference height
- The reference height of 10 m used for modelling wind variation in the atmospheric boundary layer.
- high tides
- The time at which the sea reaches its greatest depth in a particular tidal cycle; also the depth at that time.
- isothermal height
- See tropopause.
- low
- See depression.
- low tides
- The time at which the sea reaches its smallest depth in a particular tidal cycle; also the depth at that time.
- neap tides
- The time of lowest tidal range, when moon and sun work in opposition.
- obliquity
- The tilt of the Earth’s axis relative to a normal to the plane in which it orbits the sun.
- orbit
- The path followed by a body moving round another under the influence of gravity.
- peak
- The highest point of a wave.
- ripples
- Surface waves in water (or any other liquid) with an amplitude much smaller than the undisturbed depth.
- slack water
- A time when tidal currents are zero, usually coinciding with high or low tide.
- spring tides
- The time of highest tidal range, when moon and sun work together.
- stratosphere
- The upper part of the atmosphere.
- surges
- Rapid changes of sea level due to tidal effects.
- swell
- Long-wavelength oceanic waves.
- tidal bulge
- One of two areas of increased water depth, caused by the gravitational attraction of the sun and moon, which travel around the world and cause tides.
- tidal currents
- Horizontal flows of water caused by tidal depth changes.
- tidal node
- See amphidromic point.
- tidal range
- The difference in height between a high tide and the preceding or following low tide.
- tidal wave
- An ocean wave, normally caused by an undersea earthquake, which on approaching land causes a sea level change comparable to that caused by tides.
- trade winds
- The relatively constant east–west winds that blow in the tropical zones north and south of the equator.
- tropopause
- The top of the troposphere, above which the atmospheric temperature (in the stratosphere) is effectively constant. Also called isothermal height.
- troposphere
- The lower part of the atmosphere, in which most weather systems exist.
- trough
- The lowest part of a surface wave.
- tsunami
- Japanese term for a tidal wave, derived from ‘tsu’ (harbour) + ‘nami’ (wave).
- wave periodic time
- The time it takes for any point to experience a full wave cycle.
- wave speed
- The speed at which a travelling wave advances.
- wavelength
- The spatial distance over which a periodic waveform repeats (e.g. the distance between successive peaks or successive troughs).
- waves
- Any regular oscillation of a continuous medium.
- westerlies
- The relatively constant west–east winds that blow in the temperate zones further north and south of the equator than the tropical zones.