Chapter3 summery Flashcards
(32 cards)
Waves form due to: (apart from waves generated by tsunamis)
- The action of the wind blowing over the sea surface. which generate from
- wind sea: local wind, in real time
- swell or groundswell: wind that blew over the ocean surface thousands of km away up to several days before
Swell:
- AKA surface gravity waves
- Series of mechanical waves that propagate along the interface between water and air
- Long wavelength (rarely more than 150m in Mediterranean)
wavelength varies due to- Weather systems
- Size,
- Strength and
- Duration
- Size of water body
- Weather systems
- Wavelength varies from event to event (longer than 700m are a result of severe storms like tropical cyclones)
Swells and locally generated wind
- Narrower range of frequency and directions than locally generated wind because
- Swell waves have dispersed from their generation area.
they have a more defined- Shape and direction
- Swell waves have dispersed from their generation area.
Swell direction
The direction from which the swell is coming. It is measured in degrees (as on a compass), and often referred to in general directions, such as a NNW or SW swell.
Causes of swell formation
- Wind speed or strength relative to wave speed — the wind must be moving faster than the wave crest for energy transfer, stronger prolonged winds create larger waves
- The uninterrupted distance of open water over which the wind blows without significant change in direction (called the fetch)
- Width of area affected by fetch
- Wind duration — the time over which the wind has blown over a given area
- Water depth
The causes of swell formation determine
- The size of the wind waves
- Wave height (trough to crest)
- Wave length (crest to crest)
- Wave period (time interval between arrival of consecutive crests at a stationary point)
- Wave propagating direction
Fully developed sea has the maximum wave size possible for a wind of a
- Specific strength
- Duration
- Fetch
Exposure to that wind can cause
- Loss of energy due to the breaking of wave tops
- Formation of whitecaps
Wave in specific area have a
range of heights
Sea water waves is generated by
disturbances such as
- Seismic events
- Gravity
- Crossing wind
Generation of wind wave is initiated by
- Disturbances of cross wind field on the surface of the sea water
Mechanisms that explain how wind generate waves and perturbation on the surface ocean
- Kelvin-Helmholtz instability (KHI)
- Miles-phillips mechanism
Kelvin-Helmholtz instability (KHI)
- Relevant to the generation of large wavelength purturbations
Kelvin-Helmholtz instability (KHI)
- Relevant to the generation of large wavelength purturbations
Can occur when
- There is velocity shear in a single continuous fluid or
- There is a velocity difference across the interface between two fluids
Kelvin-Helmholtz instability (KHI)
- Relevant to the generation of large wavelength purturbations
Can occur when
- There is velocity shear in a single continuous fluid or
- There is a velocity difference across the interface between two fluids
Example is:
Wind blowing over the water
- The instability manifests in waves on the water surface. More generally
- Clouds
- Ocean
- Saturn’s bands
- Jupiter’s red spot
- Sun corona
KHI require
- Minimum wind speed of 6 m/s to make waves grow against the competing effect of
- Gravity and
- Surface tension
Miles phillips mechanism
- Describe how waves are generated from a flat sea using two mechanisms
- First: produce small ripples “capillary waves”
- Second: produce bigger waves “gravity waves”
- Relevant to low wind speeds and short wave length perturbations
- Involved a resonant interaction between the surface of the water and turbulent fluctuations in the air
How waves are produced in general:
Air moving over the surface of the water transmits its energy to the water.
Capillary and gravity waves:
- Capillary grow from flat sea
- Gravity wave form from sea containing capillary waves
Capillary and gravity waves:
- Capillary grow from flat sea
- Gravity wave form from sea containing capillary waves
Reason behind the naming:
Because of the restoring force
Restoring forces of capillary and gravity waves:
- Gravity in case of gravity and capillary
- Surface tension in case of capillary
Swell dissipation for short waves
- Stronger than long waves, this is why swells from distant storms are only long waves
- Dissipation of waves with periods >13s is weak but significant at the pacific ocean scale
- Long swells lose half of their energy over 20 thousand km to over 2 thousand km
- This variation is a systematic function of swell steepness (due to friction at the air-sea interface)
- Ratio of the swell height to the wavelength
- This variation is a systematic function of swell steepness (due to friction at the air-sea interface)
Swells are often created by
Storms thousands of nautical miles away from the beach where they break
The propagation of the longest swells is limited by
The shoreline