scholarly journals Using Argus Video Monitoring to Determine Limiting Factors of Aeolian Sand Transport on a Narrow Beach

2018 ◽  
Vol 6 (4) ◽  
pp. 138 ◽  
Author(s):  
Pam Hage ◽  
Gerben Ruessink ◽  
Jasper Donker

Aeolian sediment transport on beaches is responsible for dune growth and/or recovery. Models predicting potential aeolian sediment transport rates often overpredict the amount of deposition on the foredune when applied to narrow (<100 m) beaches, pointing to supply limitations. Our goal is to better understand these limitations, especially in the long-term (>years) in order to improve predicted transport volumes and the timing of transport. Here, we used 8 years of Argus video images at Egmond aan Zee, The Netherlands, in combination with routine weather data to delineate 241 limited from 467 unlimited sand transport events to explore supply-limiting factors. Our research shows that the wind is more oriented to the west (shore normal) and is generally stronger for limited transport events. This indicates that the available fetch distance is often less than the critical fetch needed for unlimited transport. This is further confirmed by the timing of the transport events, as limited events often became unlimited during low tide when the beach was the widest and fetch potentially the longest. Our results help understanding the nature of aeolian sediment transport on narrow beaches, which will hopefully lead to better predictions of annual aeolian sediment transport rates.

2020 ◽  
Vol 8 (8) ◽  
pp. 584
Author(s):  
Jorn T. Tuijnman ◽  
Jasper J. A. Donker ◽  
Christian S. Schwarz ◽  
Gerben Ruessink

Wind-blown beach sand is the primary source for the volume growth of the most seaward dune, the foredune. Strong wind events can potentially dominate long-term aeolian supply but in reality do not contribute considerably because they often coincide with a storm surge. The aim of this paper is to further our understanding of how a storm surge prevents or severely restricts aeolian supply. Using field data collected on the 1:50 sloping Egmond beach (Netherlands) in the aftermath of a 1-m storm surge, we show that the ground water in the upper beach rose to well above normal levels during the surge, which resulted in the development of a seepage face during falling tide and hence persistent saturation of the emerging beach. Using a fetch-based model, we predicted aeolian supply during the 2-day surge period to be about 66% of the potential supply. Fetch limitations imposed by the surge-induced inundation and the continuous saturation of the sand on the emerging beach both contributed to the predicted supply limitation. Our results quantitatively support earlier studies that suggested surges to be the primary condition that causes predictions of long-term potential foredune growth to overestimate measured growth.


Sensors ◽  
2018 ◽  
Vol 18 (3) ◽  
pp. 820 ◽  
Author(s):  
Alessandro Pozzebon ◽  
Irene Cappelli ◽  
Alessandro Mecocci ◽  
Duccio Bertoni ◽  
Giovanni Sarti ◽  
...  

1986 ◽  
Vol 17 (1) ◽  
pp. 30-34 ◽  
Author(s):  
R. P. Bourman

Sign in / Sign up

Export Citation Format

Share Document