Very Low Frequency (VLF) rip current pulsation investigations are still poorly documented in the literature. In this paper, we analyse data acquired during an in-situ field experiment on Truc Vert beach, on the Aquitanian coast. This beach was exposed to high energy wave conditions during a spring tide cycle and has high tidal range and gentle slope. VLF motions were observed within the surf zone, with a characteristic frequency of 6 10-4 Hz which corresponds to a 27 minute period. These VLF motions were associated with high velocity. This paper shows that the VLF velocity pulsations were larger in the inner surf zone and increased with increasing offshore wave energy. We found that the significant wave height and the velocity evolved in-...
Field observations of swash and ocean waves show that runup saturation at infragravity frequencies (...
Field observations and numerical model simulations are examined to investigate the magnitude of vort...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
The exchange of material between the surf zone and continental shelf can be driven by pulsations in ...
International audienceExperimental results on a rip formed over a heterogeneous beach with a mobile ...
Numerical computations are used to explain the presence of very low frequency motions (VLFs), with f...
International audienceAbstract A wave group-resolving model is used to investigate the driving mecha...
Observations of velocity fluctuations with periods between about 4 and 30 min, thus longer than infr...
International audienceThe Aquitanian Coast (France) is a high-energy meso-macrotidal environment exh...
longer than infragravity waves and referred to as very low frequency (VLF) surf zone motions, are de...
International audienceHeadland rips, sometimes referred to as boundary rips, are rip currents flowin...
Rip currents are the main cause of beach rescues and fatalities. Key drivers of rip current hazard a...
The dissipation of the sea-swell frequency band energy (nominally 0.09 < f less than or equal to 0.3...
[1] The origins of rip current pulsations within the infragravity frequency band (0.004–0.04 Hz) are...
International audienceWe analyze Eulerian and Lagrangian measurements of wave-induced circulation co...
Field observations of swash and ocean waves show that runup saturation at infragravity frequencies (...
Field observations and numerical model simulations are examined to investigate the magnitude of vort...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
The exchange of material between the surf zone and continental shelf can be driven by pulsations in ...
International audienceExperimental results on a rip formed over a heterogeneous beach with a mobile ...
Numerical computations are used to explain the presence of very low frequency motions (VLFs), with f...
International audienceAbstract A wave group-resolving model is used to investigate the driving mecha...
Observations of velocity fluctuations with periods between about 4 and 30 min, thus longer than infr...
International audienceThe Aquitanian Coast (France) is a high-energy meso-macrotidal environment exh...
longer than infragravity waves and referred to as very low frequency (VLF) surf zone motions, are de...
International audienceHeadland rips, sometimes referred to as boundary rips, are rip currents flowin...
Rip currents are the main cause of beach rescues and fatalities. Key drivers of rip current hazard a...
The dissipation of the sea-swell frequency band energy (nominally 0.09 < f less than or equal to 0.3...
[1] The origins of rip current pulsations within the infragravity frequency band (0.004–0.04 Hz) are...
International audienceWe analyze Eulerian and Lagrangian measurements of wave-induced circulation co...
Field observations of swash and ocean waves show that runup saturation at infragravity frequencies (...
Field observations and numerical model simulations are examined to investigate the magnitude of vort...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...