In fluid dynamics, the Iribarren number or Iribarren parameter – also known as the surf similarity parameter and breaker parameter – is a dimensionless parameter used to model several effects of (breaking) surface gravity waves on beaches and coastal structures. The parameter is named after the Spanish engineer Ramón Iribarren Cavanilles (1900–1967), who introduced it to describe the occurrence of wave breaking on sloping beaches. The parameter used to describe breaking wave types on beaches; or wave run-up on – and reflection by – beaches, breakwaters and dikes. Iribarren's work was further developed by Jurjen Battjes in 1974, who named the parameter after Iribarren.[1] [2]
The Iribarren number which is often denoted as Ir or ξ – is defined as:
\xi=
| \tan\alpha | |
| \sqrt{H/L0 |
L0=
| g | |
| 2\pi |
T2,
where ξ is the Iribarren number,
{\displaystyle\alpha}
The type of breaking wave – spilling, plunging, collapsing or surging – depends on the Iribarren number. According to, for periodic waves propagating on a plane beach, two possible choices for the Iribarren number are:
\xi0=
| \tan\alpha | |
| \sqrt{H0/L0 |
\xib=
| \tan\alpha | |
| \sqrt{Hb/L0 |
where H0 is the offshore wave height in deep water, and Hb is the value of the wave height at the break point (where the waves start to break). Then the breaker types dependence on the Iribarren number (either ξ0 or ξb) is approximately:
| breaker type | ξ0–range | ξb–range | |
|---|---|---|---|
| surging or collapsing | ξ0 > 3.3 | ξb > 2.0 | |
| plunging | 0.5 < ξ0 < 3.3 | 0.4 < ξb < 2.0 | |
| spilling | ξ0 < 0.5 | ξb < 0.4 |