2013
DOI: 10.1016/j.margeo.2013.05.005
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An insight into headland sand bypassing and wave climate variability from shoreface bathymetric change at Byron Bay, New South Wales, Australia

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Cited by 68 publications
(67 citation statements)
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“…For example, Ten Mile Beach ( Figure 1B) Because many beaches along the northern NSW coast are connected via a northward-directed littoral sand transport system [40], temporary or persisting divergences in transport rates can also drive periodic beach erosion or ongoing shoreline recession. Periodic erosion may occur where wave climate variability supports only intermittent sediment bypassing of prominent headlands [41,54]. On the other hand, persistent and ongoing shoreline recession may result from a long-term sediment budget imbalance within a coastal sediment compartment.…”
Section: Exposure To Coastal Erosionmentioning
confidence: 99%
“…For example, Ten Mile Beach ( Figure 1B) Because many beaches along the northern NSW coast are connected via a northward-directed littoral sand transport system [40], temporary or persisting divergences in transport rates can also drive periodic beach erosion or ongoing shoreline recession. Periodic erosion may occur where wave climate variability supports only intermittent sediment bypassing of prominent headlands [41,54]. On the other hand, persistent and ongoing shoreline recession may result from a long-term sediment budget imbalance within a coastal sediment compartment.…”
Section: Exposure To Coastal Erosionmentioning
confidence: 99%
“…Sediment connectivity via littoral and shoreface sand transport means that many NSW beaches cannot be considered isolated features that vary independently from surrounding beaches (Goodwin et al, 2013). Rather, most beaches are elements of larger sediment-sharing systems, and respond to the redistribution of sand within the system due to evolving forcing conditions, such as the energy climate or sea level (Cowell et al, 2003).…”
Section: Regional Settingmentioning
confidence: 99%
“…However, four processes contribute to the problem. Three of these are: (1) a decadal-scale sand-supply deficit in the longshore sand-transport rate bypassing Cape Byron and which is associated with fluctuations in wave climate (Goodwin, Freeman and Blackmore 2013); (2) an increase in incident easterly storm-wave power; and (3) the interruption of natural sand transport alongshore by the Jonson Street carpark (Byron Bay Central Business District (CBD) -see Figure 1). …”
Section: The Byron Bay Backgroundmentioning
confidence: 99%