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instrument / verified-clean
Wave Energy Flux Estimator
The current ledger marks this instrument verified clean within the source-bound verification corpus.
Inspectable records
Ledger state
The current ledger marks this instrument verified clean within the source-bound verification corpus.
- Area
- Earth & Space (astronomy, orbital mechanics, meteorology, geology, geodesy, oceanography)
- Tranche
- tranche-5
- Evidence ID
- t5-143
- Ledger rows
- 1
No ledger note is attached.
Review findings
The arithmetic is correct under SI units with rho = 1025 kg/m^3, g = 9.81 m/s^2, significant wave height Hs, and energy period Te. Resolve the period definition and replace or revise the sinusoidal honest label before release.
Formula and scope findings
- The formula is standard for significant wave height Hs combined with energy period Te (or an equivalent spectral period), but the specification only says generic wave period; that period definition is ambiguous.
- The honest label says sinusoidal wave approximation, but the 1/(64π) coefficient is the standard deep-water irregular-wave result using significant wave height. For a regular sinusoidal wave using crest-to-trough height H, the corresponding coefficient is 1/(32π).
- The deep-water applicability constraint is not specified. A depth input or an explicit requirement such as depth being at least approximately half the wavelength is needed to verify the approximation.
Unit assumptions
- Use seawater density rho = 1025 kg/m^3 unless another value is explicitly selected.
- Use gravitational acceleration g = 9.81 m/s^2.
- Significant wave height Hs must be in metres.
- Wave period Te must be in seconds; minutes must be converted by multiplying by 60.
- The formula produces power in watts per metre of crest; divide by 1000 to report kW/m.
- The deep-water assumption requires sufficiently large depth relative to wavelength, commonly depth greater than about half the wavelength.
Boundary hardening
BREAK_CLAIMED · SELF_FLAGGED
The plain-arithmetic implementation can overflow to Infinity for extreme finite inputs, and the specification provides no alternate formula or depth input for the shallow/intermediate-water branch even though the advertised formula is explicitly limited to deep water.
Errata and corrections
No applied erratum is attached to this unique-name record.
Inspectable example
4 review vectors are recorded. One source-bound sample is shown below.
{
"inputs": {
"significant_wave_height_m": 2,
"energy_period_s": 8,
"seawater_density_kg_m3": 1025,
"gravity_m_s2": 9.81
},
"expected_outputs": {
"power_kW_per_m": 15.6994
},
"working": "g^2 = 9.81^2 = 96.2361. rho*g^2 = 1025*96.2361 = 98642.0025. 64*pi = 201.06193. Coefficient = 98642.0025/201.06193 = 490.60507 W/m per (m^2*s). Hs^2*Te = 2.0^2*8.0 = 4*8 = 32. P = 490.60507*32 = 15699.3623 W/m. Convert: 15699.3623/1000 = 15.6994 kW/m."
}Related workflows
No source-defined multi-instrument workflow membership is recorded.
Sources and evidence
These pointers bind the page to evidence. They do not grant authority or collapse verification into deployment.
VERIFIED_LEDGER.json · VERIFIED_CLEANevidence-tranche5/tranche5-results.jsonBOUNDARY_HAZARD_CATALOG.json