OBSERVATION CHAMBER / ACTIVE

Spectral Wave Surface Field

Combine spectral components on a surface and observe how wavenumber, phase, dispersion, and group velocity shape a moving wave packet.

wave / dispersion Observation Model

66 / FIELD · DISPERSION

Surface, envelope, spectrum

Read a fixed-depth linear gravity-wave field from one shared model.

PAUSED

The solid trace is surface η, the dashed trace is the narrow-band envelope, and the lower band is the component spectrum.

The field is paused. Use PLAY or STEP to advance time.

Mode
SUPERPOSE
Depth h
1.80 m
Components
5 / 8
Sample cap
1,200 / 20,000

DISPERSION READOUT

Readouts

PASS
Wavenumber k
0.800 1/m
Wavelength λ
7.854 m
Angular frequency ω
2.77 rad/s
Phase velocity cp
3.46 m/s
Group velocity cg
1.88 m/s
cg / cp
0.54
Envelope center
0.00 m
Measured speed
1.88 m/s
Linear validity
PASS · ka 0.03 · a/h 0.02

MODEL CHECKS

Deterministic acceptance

Check the equation and numerical derivative with fixed samples.

PASS
CHECKVALUELIMITRESULT

OBSERVATION CONTRACT

Observation contract

η = Σ A cos(kx − ωt + φ), ω = √(gk tanh kh). No point sources, boundary reflections, wind/current, breaking, or shoreline CFD.

WHAT TO WATCH

Read the ratio and packet

SHALLOW drives cg/cp toward 1; DEEP drives it toward 0.5. In SUPERPOSE, the envelope center moves at group velocity.

MODEL NOTE

Browser-local model

Canvas 2D observation with at most 8 components and 20,000 samples. Inputs and images stay local.

OBSERVATION POLICY

This field runs a browser-local spectral wave-surface model. Wavenumbers, phases, calculations, and images are not uploaded. It is not an ocean forecast, sonar, or physical wave measurement.