Waves
Wave Terminology
H = Height A = Amplitude = 1/2H L = λ = Wave Length ( distance 2 consecutive crests) T = Wave Period (Time between 2 consecutive crests) f = Wave Frequency = 1/T (# waves/sec) C = Wave Speed or Celerity = L/T (m/s) H/L = Wave Steepnes –Waves Break = H/L = 1/7
Wave Motion & Energy
Wave Spectrum
Ocean surface waves
Wind Waves What influences wave size? –Wind Speed H, L, T –Duration of wind Maximum H –Fetch Maximum H –Wave Height (H) –Wave Interference
i.e. Effect of wind speed on H
Wave Interference
Wave Interference – Area of Fetch
Fetch Area
Wave formation in storms Fetch Area: Chaotic (Rogue Waves)
Wave Speed (Deep Water) C = L/T = 1.25 * √L L = 1.56 *T 2 Slow Wave Speed –long Period (T) –Short Length (L) Fast Wave Speed –Short Period (T) –Long Length (L)
Wave Dispersion Outside Fetch Area: L, T & C remain constant
Waves and Currents
Reduction speed = Increase steepness C=L/T Steepness = H/L
Figure 9.9
Orbital Motion
Shallow Water Waves Deep Water Waves (Depth > L/2) C = L/T = 1.25 * √L Intermediate Waves (L/2 > D > L/20) C ~ D, L Shallow Water Waves (d < L/20) C = 3.13 * √D
Shallow Water Waves
Shallow Water Waves (d < L/20) C = 3.13 * √D C = L / T –C (speed) diminishes in shallow water –T (period) remains constant –.. So L (Length) must also diminish –C & L depend on depth
Figure 9.12
Shallow Water Wave Height
Shallow Water Waves When D<L/20 Speed decreases ~ D Length decreases ~ D Height increases ~ D Wave steepness (H/L) –Increases very quickly H/L = 1/7 Waves break
Wave Difraction
MUNDAKA VIDEO
Teahupoo – Tahiti surging breaker long wavelengths steep slope
Teahupoo Tahiti
Pipeline - Oahu plunging breaker
Folly Beach - SC plunging breaker moderate slope, small wavelength
Rip Currents
Tsunami Waves Earthquakes L ~ 100 – 200 Km P ~ minutes Shallow Water Waves C over 4000m depth = 200 m/s = 720 km/h Refracted by topography Height at sea = 1-2 meters Dangerous in shallow water H~10’s m ; T~10-30 min.
Figure 9 p264 (figure 1)
Figure 9.24
Wave trains or ‘sets’ Train Speed = ½ wave speed = 1/C