Unsteady waves Flashcards
Cause of nonlinearity
-driven by nonlinear FSBC
-larger for steeper waves
Formation of regular waves
-1 free wave therefore 1 phase velocity
-applying a moving frame of reference would produce a steady graph
Formation of irregular waves
-for >= 2 bound waves so there is no unique phase velocity
-real waves deform with both space and time
load predictions
-loads reliable only when the model accurately predicts wave particle kinematics
*drag domination -> F is directly proportional to u2
*stokes is easy to apply but “nonphysical” so inaccurate
-failure is often assessed at the bed as shear or overturning moments
*only loads above the failure surface are considered
*calibration is applies to that surface but requires prior knowledge of the failure mode
wave types
swell
- narrow range of low f
- unidirectional and steady-ish
wind
-bread range of high f
-multidirectional with irregularity
-+-20 degrees of directional spread
linear random wave theory
-sum the linear regular wave solution for eta and u
*applies the dispersion equation
-based in the fourier analysis of a measured wave and should only be applied to the free linear waves
Accuracy
- nonlinear effects are laegrest near the surface where u and partial du/dt are at their max so this has a big impact on the F/M predctions
-should be applied to the the surface level but errors increase as it is approached
-high f contamination
High f contamination
-small amplitude, high f waves are extrapolated to heights far above their amplitude
-method doesnt account for high f waves on low f ones
-this is all an issue with effective depth
wheeler stretching
-empirically reduced velocity at SWL but doesnt satisfy mass continuity and is insufficient to model real fluid flow
-basically incorrect
z* = (z - eta(t)) / (1+eta(t)/d)
Nonlinear random wave theory
Bound waves tend to be more significant than the regular waves
For a high f wave on low f wave, both free
-long wave is unchanged
-short wave has higher a and shorter L in the long waves peak but shallower and longer in its trough
* change can be treated as a new bound wave needed to satisfy FSBC
*amplitude modulation as follows
g’ = g + (partial d2eta/dt2)_longwave
mgh = constant, so change in gravity drives change in H
Spectra for random wVe theory application
cant separate bound in measure/calculated spectra
-for bound c not = omega/k so the dispersion equations doesnt apply
-1st order has no bound terms
- >= 2nd order has stokes terms with all up to >=2 wave coupling
-2nd order can use bispectral analysis to ID 2 wave coupling
Second order random wave theory
-sums the interactions from all possible free wave pairs
-difficult to use for measured data