Abstract
The response of headland protected beaches to storm events is complex and strongly site dependent. In this study, we investigated the response of several headland protected beaches in Noosa, Australia to a tropical cyclone event. Pre and post topographical surveys of all beaches were completed using both pole-mounted RTK-GNSS and structure-from-motion (SfM)-derived elevation models from survey-grade drone imagery to assess sediment volume differentials. Coastal imaging was used to assess shoreline development and identify coastal features while a nearshore wave model (SWAN) was used to project waves into the study site from a regional wave buoy. Obliquely orientated swells drive currents along the headland with sediment being eroded from exposed sites and deposited at a protected site. Elevated sea-levels were shown to be a strong force-multiplier for relatively small significant wave heights, with 10,000 m3 of sediment eroded from a 700 m long beach in 36 h. The SWAN model was adequately calibrated for significant wave height, but refraction of swell around the headland was under-represented by an average of 16.48 degrees. This research has coastal management implications for beaches where development restricts natural shoreline retreat and elevated sea states are likely to become more common.
Highlights
Headland protected beaches make up the majority of Australia’s favourite beach destinations, with locations such as Byron Bay, Burleigh Heads, Bondi Beach and Noosa Main Beach, all frequently within the Australia’s top 10 beach destinations [1]
The cyclone track of Tropical cyclone (TC) Oma (Figure 3) shows that the storm passed to the east and south of Noosa, with the maximum significant wave height (Hs ) of the event being from the south east
While TC Oma did produce substantial erosion at Noosa Main Beach, an analysis of the wave height and storm surge conditions indicate that this storm did not produce unusually large local significant wave height and storm surge conditions indicate that this storm did not produce conditions
Summary
Headland protected beaches make up the majority of Australia’s favourite beach destinations, with locations such as Byron Bay, Burleigh Heads, Bondi Beach and Noosa Main Beach, all frequently within the Australia’s top 10 beach destinations [1]. Headland protected beaches often avoid the impacts from predominate major storm events compared to neighbouring open coast beaches [4,5] When impacted, they are often vulnerable to relatively high erosion, as a result of wave energy dissipating directly on the beach face due to a lack of offshore bars [6,7]. They can experience prolonged recovery times following an event, mainly as a consequence of the headland inhibiting the flow of longshore sediment needed for recovery [8,9,10]
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