{"refrec":{"BRefID":317931,"RR":"<b>Montreuil, A.-L.; Chen, M.; Brand, E.; Dan, S.</b> (2017). Monitoring aeolian activity during a storm event using a video system, <b><i>in</i></b>: <i>Proceedings of Coastal Dynamics 2017, 12-16 June 2017, Helsingør, Denmark.</i> pp. 461-470","BEntID":311368,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: <i>Proceedings of Coastal Dynamics 2017, 12-16 June 2017, Helsingør, Denmark.</i> pp. 461-470","DocTypID":17,"DocType":"Book chapters","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Montreuil, A.-L.; Chen, M.; Brand, E.; Dan, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Montreuil, A.-L. <i>et al.</i>","Englishabstract":"Aeolian sand transport was assessed from an Argus camera system located on a macro-tidal beach along the Belgian coast over a period of 4 days covering a storm surge. Over the study period, observed sand transport event occurred for 9.5% of the time when strong high oblique onshore wind (9.8m/s) combined with a water level below 3.75m TAW moved sand to the beach. Measured post-storm topographic profiles indicated an accretion on the total beach upper beach of 0.70m3/m, which was in agreement with the estimated potential sand supply of 0.91m3/m for the observed sand transport event and expected night transport events. Thus, there was a narrow temporal window in which sediment can be supplied to the beach before and after the storm surge. 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