Waves
Source
·
Wind (radiated all directions)
·
Coastal landslides, calving icebergs (splash waves)
·
Seafloor motion, turbidity current, volcano
eruption, fault slippage (seismic waves / tsunami)
·
Moon sun gravity pull (tide)
·
Tidal motion, turbidity, ships
·
Diff density (internal waves)
ü Water–water
interface
ü Height > 100 m
Property
·
Ripples / capillary waves (L < 1.74 cm)
·
More energy, becomes gravity waves > 1.74 cm
·
Wave period, T, interval between successive crests
·
Still water lvl = 0 energy lvl (halfway between
crest & trough)
·
Wave steepness = H /L
·
Steepness > 1/7; unsupportable & breaks
·
Water x travel, waveform travels; energy passed
circularly (Circular Orbital Motion)
·
Diameter = height
·
Wave base = depth of negligible circular orbits; ½
of L
·
High L, high speed
·
Shallow-water waves depth < 1/20 L
Transitional waves
·
Between shallow & deep
·
L = 2x – 10x depth
Energy depend on
·
Speed, period & distance of wind
·
Speed reduce, wave steepness reduce, become long
crested waves (swells)
Speed depend on
·
Depth & wavelength
Swells
·
Uniform, symmetrical waves radiate from origin
·
Little energy loss; transport energy
·
Possible @ distant shoreline with x wind
Interference Pattern
·
Diff storm swells join
·
Constructive
·
Destructive
·
Mixed Interference
ü 2 swells of
various heights & lengths
ü Form diff
sequence of high & low waves
ü Irregular wave
pattern when swell approach shore
ü Large hazardous
waves @ open ocean
·
Deep waves toward shallow water; Depths < L/2 à transitional
wave
Speed
reduce, wavelength reduce, energy contribute height, steepness rise, wave breakSurging breaker – abrupt beach slopeUnnoticed @ deep water till shore
Breaker Types
·
Spilling breaker – gradual beach slope
·
Plunging breaker – steep beach slope
Tsunami
·
Sudden sea topography change
·
Fault slippage / avalanche /
eruptions
·
Displace crust, earthquakes,
seafloor rupture
·
Ocean basin volume change
·
L > 200 km (shallow-water
wave everywhere)
·
700 km/hr @ open ocean; height
0.5 m
No comments:
Post a Comment