H7 Flashcards
wave
displacement of energy, not of medium (water stays on more or less the same place)
parts of a wave (4)
- wave height (golfhoogte)
- crest (golftop)
- wave length (golflengte)
- trough (golfdal)
wave period
time between two consecutive crests that pass by the same point (one wave length)
7 types of waves (ordered from lowest to greatest in wave period)
- capillary waves (capillaire)
- chop waves (kalme golven)
- swell waves (surfgolven)
- seiches (meteotsunami)
- tsunamies (tsunami’s)
- tidal waves (getijdengolven)
- internal wave (onderwater golven)
the size and type of wave is dependent on:
- wind speed
- duration of the wind
- fetch (strijklengte)
- initial situation
what does higher wind speed mean?
the longer the wave length, wave period and height
be each windspeed is there a:
- average wave height, length and period
- significant height
- determinant for damage on e.g. ships and erosion of coast lines
wave height
the significant wave height is the average wave height, from trough to crest, of the highest 33% (1/3) of the wave height during a timed interval. The significant wave height is, as a rule of thumb, the height that people perceive visually.
progressive waves (lopende golven)
energy moves, water mass moves little/does not move
how do water molecules move in the movement of waves?
vertical, circle forming motion (orbital motion).
- diameter of the circle increases with wave size
- diameter of the circle decreases with depth
- decreasing diameter of the circle (orbital motion) with increasing distance under the water surface.
- under 0,5L (the half wave length) there is no movement more of the wave
is there net water transport?
- orbits are not always closed, therefore, there is net water transport
- in open ocean this is negligible, but in deep water it has more effect
what happens to the orbits if the water is deeper than the half wave length (wave base)?
the orbits are circular and there is no influence on the bottle of the wave or otherwise
what happens to the orbits if the water is shallower than the half wave length (wave base)?
the orbits are elliptical and there is an influence on the bottom of the wave and otherwise.
calculation for the speed of a wave
C = L/T
C= celerite, or wave speed L= wave length T= wave period
what is wave speed dependent on?
wave length, wave period and wave type (deep wave, shallow wave, medium wave)
how do waves exist in new ocean?
many waves, chaotic sea
how do waves exist in living ocean?
deinende waves, regular
how do waves exist in a dying ocean?
breaking waves
what happens during the breaking of waves to wave length?
decreases
what happens during the breaking of waves to wave speed?
decreases
what happens during the breaking of waves to the wave height
increases
do longer waves travel faster than shorter waves? why or why not?
yes. wave speed (celerity) increases as soon as wave length increases. Therefore, longer waves are faster than shorter waves
waves in deep water
how deeper the water, the bigger the interaction between waves and the bottom. By increase of the depth, is there also and increase of the wave speed and wave length. wave heigh increases. If the H/L is greater than or equal to 1/7, then the wave becomes unstable and breaks.
how to calculate wave speed in deep water
C = square root of gd
G=gravitational acceleration (zwaartekrachtversnelling)
D=water depth
Refraction
Reflection involves a change in direction of waves when they bounce off a barrier. Refraction of waves involves a change in the direction of waves as they pass from one medium to another. Refraction, or the bending of the path of the waves, is accompanied by a change in speed and wavelength of the waves.
types of breaking waves
- spilling breaker
- plunging breaker
- surging breaker
standing wave
- movement is not horizontal
- move back and forth around a fixed point called a node
- a standing wave in a lake, harbour or estuary is a seiche (meteotsunami)
underwater waves originating from pycnocline:
- contact between water layers of different densities
2. comparable with contact between water layer and air layer
how are underwater waves measured?
the course of temp of the water indicates extreme underwater waves
tsunamies
- tsunamies are also called flood waves
- the occur through, for example, volcanic eruptions and earthquakes
- they are not related to tides
process of tsunami creation:
- start with low wave, long wave period and long wave lengths
- in the open ocean, celerity is 760km/hour
- wave heigh starts low (around 2m) and grows to greater than 10m