Lidar observations of the swash zone of a low-tide terraced tropical beach under variable wave conditions : the Nha Trang (Vietnam) COASTVAR experiment

2020

Article référencé dans le Web of Science WOS:000539274600003

Almeida L. P., Almar Rafaël, Blenkinsopp C., Senechal N., Bergsma E., Floc'h F., Caulet C., Biausque M., Marchesiello Patrick, Grandjean P., Ammann J., Benshila R., Thuan D. H., da Silva P. G., Viet N. T.

Journal of Marine Science and Engineering, 2020, 8 (5), p. art. 302 [ p.]

A field experiment was conducted at a tropical microtidal intermediate sandy beach with a low tide terrace (Nha Trang, Vietnam) to investigate the short-term swash-zone hydrodynamics and morphodynamics under variable wave conditions. Continuous 2D Lidar scanner observations of wave height at the lower foreshore, subsequent run-up and swash-induced topographic changes were obtained. These data were complemented by detailed real-time kinematic GPS topographic surveys. Variable wave and tide conditions were experienced during the field experiment with relatively large swell waves (offshore significant wave height, H-s = 0.9 m to 1.3 m; peak wave period, T-p = 8 to 12 s) concomitant with spring tides at the beginning of the period, followed by mild wind waves (offshore H-s under 0.5 m and T-p 5 s) and neap tides. This resulted in the following morphological sequence: berm erosion followed by rapid neap berm reformation and beach recovery within a few days. New insights into the link between intra-tidal swash dynamics and daily beach profile evolution were found using the Lidar dataset. While waves directly cause morphology changes on a wave-by-wave basis, tidal levels were found to be a key factor in determining the morphological wave-effect (accretive or erosive) due to modulated interaction between surf and swash hydro-morphodynamics.

Limnologie physique / Océanographie physique [032] ; Géologie et formations superficielles [064] ; Télédétection [126]

VIET NAM ; NHA TRANG

Fonds IRD [F B010078203]

fdi:010078203