2010Journal of Geophysical Research AtmospheresRequires access

Nearshore wave height variation in unsaturated surf

Hannah E. Power, Michael G. Hughes, Troels Aagaard, Tom E. Baldock

Open publisher page 52 citations

Abstract

The nearshore evolution of wave height is presented from field observations during unsaturated surf conditions from 10 different beaches characterized by microtidal conditions and predominantly swell‐dominated wave climates. Wave evolution is presented in terms of wave height to water depth ratio (γ) for comparison with previous data from saturated surf. Both conventional time‐averaged (γrms) and a new wave‐by‐wave analysis (γw) are performed. Values of γ increase with increasing offshore wave height, indicating unsaturated surf. The observations show a variation in γ values from near constant values in the mid surf zone to rapidly and asymptotically increasing γ values in the inner surf zone. In contrast to previous data from saturated surf, γ shows no dependence on either the absolute beach slope or the relative beach slope β/k . The skewness of the distributions of γw is consistent with waves that are not depth limited. The inner surf zone wave heights are approximately equally dependent on the water depth and offshore wave height. The previous observations of γ from saturated surf are shown to be consistent with a terminal bore height at the shoreline which is in excellent agreement with a previously derived value for the Miche parameter. In contrast, for the present unsaturated surf conditions, the terminal bore height at the shoreline can be approximated by Hb ≈ 0.12Ho, which is consistent with recent laboratory data sets.

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What this paper is about

The nearshore evolution of wave height is presented from field observations during unsaturated surf conditions from 10 different beaches characterized by microtidal conditions and predominantly swell‐dominated wave climates. Wave evolution is presented in terms of wave height to water depth ratio (γ) for comparison with previous data from saturated surf. Both conventional time‐averaged (γrms) and a new wave‐by‐wave analysis (γw) are performed. Values of γ increase with increasing offshore wave height, indicating unsaturated surf. The observations show a variation in γ values from near constant values in the mid surf zone to rapidly and asymptotically increasing γ values in the inner surf zone. In contrast to previous data from saturated surf, γ shows no dependence on either the absolute beach slope or the relative beach slope β/k . The skewness of the distributions of γw is consistent with waves that are not depth limited. The inner surf zone wave heights are approximately equally dependent on the water depth and offshore wave height. The previous observations of γ from saturated surf are shown to be consistent with a terminal bore height at the shoreline which is in excellent agreement with a previously derived value for the Miche parameter. In contrast, for the present unsaturated surf conditions, the terminal bore height at the shoreline can be approximated by Hb ≈ 0.12Ho, which is consistent with recent laboratory data sets.

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Available abstract

The nearshore evolution of wave height is presented from field observations during unsaturated surf conditions from 10 different beaches characterized by microtidal conditions and predominantly swell‐dominated wave climates. Wave evolution is presented in terms of wave height to water depth ratio (γ) for comparison with previous data from saturated surf. Both conventional time‐averaged (γrms) and a new wave‐by‐wave analysis (γw) are performed. Values of γ increase with increasing offshore wave height, indicating unsaturated surf. The observations show a variation in γ values from near constant values in the mid surf zone to rapidly and asymptotically increasing γ values in the inner surf zone. In contrast to previous data from saturated surf, γ shows no dependence on either the absolute beach slope or the relative beach slope β/k . The skewness of the distributions of γw is consistent with waves that are not depth limited. The inner surf zone wave heights are approximately equally dependent on the water depth and offshore wave height. The previous observations of γ from saturated surf are shown to be consistent with a terminal bore height at the shoreline which is in excellent agreement with a previously derived value for the Miche parameter. In contrast, for the present unsaturated surf conditions, the terminal bore height at the shoreline can be approximated by Hb ≈ 0.12Ho, which is consistent with recent laboratory data sets.

Key concepts: Surf zone, Wave setup, Significant wave height, Geology, Wave height, Submarine pipeline, Shore, Swell

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