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

Almeida L.P. Instituto de Oceanografia, Universidade Federal do Rio Grande (FURG), Rio Grande, 96203-900, Brazil|
Viet N.T. | da Silva P.G. | Thuan D.H. | Benshila R. | Ammann J. | Marchesiello P. Faculty of Civil Engineering, Thuyloi University, Hanoi, 116705, Viet Nam| Caulet C. School of Geography and Environmental Science, Ulster University, Coleraine, Northern Ireland, BT52 1SA, United Kingdom| Blenkinsopp C. Department of Architecture and Civil Engineering, University of Bath, Bath, BA2 7AY, United Kingdom|

Journal of Marine Science and Engineering Số 5, năm 2020 (Tập 8, trang -)

ISSN: 20771312

ISSN: 20771312

DOI: 10.3390/JMSE8050302

Tài liệu thuộc danh mục: ISI, Scopus

Article

English

Tóm tắt tiếng anh
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, Hs = 0.9 m to 1.3 m; peak wave period, Tp = 8 to 12 s) concomitant with spring tides at the beginning of the period, followed by mild wind waves (offshore Hs under 0.5 m and Tp 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. � 2020 by the authors.

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