Articles | Volume 24, issue 11
https://doi.org/10.5194/nhess-24-4049-2024
https://doi.org/10.5194/nhess-24-4049-2024
Research article
 | 
26 Nov 2024
Research article |  | 26 Nov 2024

New insights into combined surfzone, embayment, and estuarine bathing hazards

Christopher Stokes, Timothy Poate, Gerd Masselink, Tim Scott, and Steve Instance

Related authors

Development of a National-Scale Rip Current Forecast for Aotearoa New Zealand
Christopher Stokes, Juliana Albertoni de Miranda, Tim Scott, Gerd Masselink, and Adam Wooler
EGUsphere, https://doi.org/10.5194/egusphere-2026-3638,https://doi.org/10.5194/egusphere-2026-3638, 2026
This preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).
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Cited articles

Aagaard, T., Greenwood, B., and Nielsen, J.: Mean currents and sediment transport in a rip channel, Mar. Geol., 140, 25–45, https://doi.org/10.1016/s0025-3227(97)00025-x, 1997. 
Allen, G. P.: Relationship between grain size parameter distribution and current patterns in the Gironde estuary (France), J. Sediment. Res., 41, 74–88, https://doi.org/10.1306/74d721ee-2b21-11d7-8648000102c1865d, 1971. 
Austin, M., Scott, T., Brown, J., MacMahan, J., Masselink, G., and Russell, P.: Temporal observations of rip current circulation on a macrotidal beach, Cont. Res., 30, 1149–1165, https://doi.org/10.1016/j.csr.2010.03.005, 2010. 
Austin, M. J., Scott, T. M., Russell, P. E., and Masselink, G.: Rip current prediction: Development, validation, and evaluation of an operational tool, J. Coastal. Res., 29, 283–300, https://doi.org/10.2112/jcoastres-d-12-00093.1, 2013. 
Austin, M. J., Masselink, G., Scott, T. M., and Russell, P. E.: Water-level controls on macro-tidal rip currents, Cont. Shelf Res., 75, 28–40, 2014. 
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Currents at beaches with an estuary mouth have rarely been studied before. Using field measurements and computer modelling, we show that surfzone currents can be driven by both estuary flow and rip currents. We show that an estuary mouth beach can have flows reaching 1.5 m s−1 and have a high likelihood of taking bathers out of the surfzone. The river channels on the beach direct the flows, and even though they change position over time, it was possible to predict when peak hazards would occur.
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