Waves
By Norwegian Dynamics · March 2026
Waves are the fundamental driver of vessel motion and, consequently, the reason heave compensation exists. Understanding wave characteristics — height, period, and spectral distribution — is essential for specifying compensators, planning marine operations, and determining operational weather windows.
Key Wave Parameters
Ocean waves are irregular and random, but they can be described statistically using a few key parameters:
- Significant wave height (Hs) — The average height of the highest one-third of waves. This is the standard measure of sea severity used in offshore engineering and corresponds roughly to what an experienced observer would estimate as the wave height.
- Peak spectral period (Tp) — The wave period at which the wave energy spectrum has its maximum. Typical values range from 5 seconds in sheltered waters to 15+ seconds in open ocean swell.
- Zero-crossing period (Tz) — The average period between successive upward zero crossings of the sea surface elevation. Related to Tp by factors that depend on the spectral shape.
Both Hs and Tp are critical inputs for heave compensator design — Hs determines the required stroke, and Tp influences the dynamic response and resonance avoidance strategy.
Wave Spectra
Because ocean waves are irregular, engineers describe them using a wave energy spectrum — a function showing how wave energy is distributed across frequencies. Two standard spectral models are widely used in offshore engineering:
- Pierson-Moskowitz (PM) — Describes a fully developed sea in deep water, defined by Hs alone. Suitable for open ocean conditions where wind has blown over a long fetch for an extended period.
- JONSWAP — A modification of the PM spectrum with an additional peak enhancement factor (γ, typically 1.0–7.0). Represents a developing sea with a sharper spectral peak. The default γ = 3.3 is commonly used for North Sea conditions.
The choice of spectrum affects the predicted vessel motions and, consequently, the crane tip heave that the compensator must absorb. JONSWAP spectra with high γ values concentrate energy in a narrow frequency band, which can be more challenging for resonance avoidance.
Sea States and Operational Limits
Offshore operations are planned around sea state forecasts that specify Hs and Tp (and sometimes directional spreading and swell components). Each marine operation has a defined limiting sea state — the maximum Hs at which the operation can proceed safely.
The operational limit is typically governed by the most sensitive phase of the operation — often the splash zone crossing. Heave compensation directly increases this limit by reducing dynamic loads, extending the operational weather window and reducing costly waiting-on-weather time.
For example, a subsea lift without heave compensation might be limited to Hs = 1.0 m, whilst the same operation with a well-designed passive heave compensator could proceed in Hs = 2.0–2.5 m. This can make the difference between a feasible operation and one that requires an impractically calm weather window.
Waves and Compensator Specification
When specifying a heave compensator, the wave environment determines several key requirements:
- Compensator stroke — Sized to accommodate the maximum crane tip heave amplitude, derived from Hs and the vessel’s heave RAO.
- Piston velocity — Driven by the combination of heave amplitude and wave period; shorter periods require faster compensator response.
- Natural period — The compensator must be tuned so its natural period avoids the dominant wave period range, preventing resonance amplification.
- Damping — Sized to control response near resonance whilst maintaining efficiency at typical operating periods.
Norwegian Dynamics provides engineering support to match compensator specifications to site-specific wave data. Whether using the RIGEL for cost-effective operations or the ANTARES for demanding variable conditions, correct wave characterisation is the foundation of effective heave compensation design.
