Abstract

Accurate knowledge of the sediment budget of a coastal cell is necessary for coastal management and predicting long-term coastal change. An important component in the sediment budget of many wave-dominated embayed coastlines is the amount of sediment that bypasses rocky headlands, which present partial barriers to alongshore transport. As yet, there is no universal method for estimating bypass rates. Here we show that wave-forced bypassing of an isolated headland can be estimated using a parameterisation of wave conditions, shoreface slope, sediment size, headland toe-depth and cross-shore extent. XBeach was used to simulate instantaneous rates of alongshore flux off the apex of an idealised and isolated headland, with >1100 simulations, testing various wave and morphological factors. Key variables were headland cross-shore extent as the ratio of toe-depth to bed slope (XH = htoe/tanβ) and surfzone extent as a function breaking depth and slope (Xs = hb/tanβ). The critical ratio controlling bypassing was found to be XH/XS (equivalent to htoe/hb, for an idealised headland). Bypass is predicted as: Qbypass = Q0 f(XH/XS); where Q0, the alongshore transport rate immediately updrift of the headland, is based on an existing expression (Van Rijn, 2014) and f(XH/XS) is a negative exponential function. This formulation accurately replicated bypass rates modelled by XBeach, generally to within a factor of two. Headland shape was found to be a lower-order control on bypass and was excluded from the parameterisation. Preliminary analysis suggests the expression may also be applied to groynes, though more specific testing is required. Once adapted to time-varying wave and water levels, the expression succesfully predicted bypass rates for three observed headlands over a single event. Best results were obtained using measured toe-depth to parameterise headland morphometry. Further field data are required for robust calibration, in particular for large and complex headlands that vary substantially from the idealised model used for development. The bypass expression can be used to provide a first-pass estimate of wave-forced bypassing for a wide-range of headland types; this will be of use to coastal managers, scientists and engineers working on rocky and embayed coastlines.

Highlights

  • A critical task for coastal researchers is to predict long-term patterns of coastal change, including the impacts of sea-level rise

  • One important component of the sediment budget that is often poorly constrained on rocky and embayed coastlines relates to the transport of sediment around headlands that border coastal embayments, defined as headland bypassing [3,4]

  • Bypassing rates are critical to assessing sediment budgets on embayed coastlines [5], and headlands exist in a wide range of sizes and morphologic configurations

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Summary

Introduction

A critical task for coastal researchers is to predict long-term (decadal to centennial) patterns of coastal change, including the impacts of sea-level rise. Current one-line models can be used to determine groyne bypassing, with an assumed level of permeability [8] These methods do not provide an instantaneous bypass rate estimate for a headland where the toe (Fig. 1), defined as the most seaward and deepest extent of the non-erodible headland, is in relatively deep water and bypassing is expected to occur sporadically during high-wave events. In these scenarios, the total level of bed change off the headland may be barely detectable [8], despite the presence of strong currents and energetic wave conditions [10], indicating that sediment transport must be occuring. Generalised formulas are available for determining rates of alongshore transport (e.g., CERC equation, [11]; Van Rijn, [12]); yet, no method exists to adjust the instantaneous rate of longshore transport to account for the presence of a headland, let alone headlands of various topographic configurations

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