FN Archimer Export Format
PT J
TI Water Level Modulation of Wave Transformation, Setup and Runup over La Saline Fringing Reef
BT 
AF Bruch, William Sami
   Cordier, Emmanuel
   Floc'h, France
   Pearson, Stuart Grant
AS 1:1,2;2:3;3:1;4:4,5;
FF 1:;2:;3:;4:;
C1 Univ Brest, CNRS, Géo-Océan, UMR6538, Plouzané, France
   Ecole Centrale de Nantes, CNRS, LHEEA, UMR6598, Nantes, France
   Observatoire des Sciences de l’Univers de La Réunion (OSU-R), UAR3365, Saint Denis, France
   Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, The Netherlands
   Department of Applied Morphodynamics, Deltares, Delft, The Netherlands
C2 UBO, FRANCE
   ECOLE CENT NANTES, FRANCE
   UNIV LA REUNION, FRANCE
   UNIV DELFT, NETHERLANDS
   DELTARES, NETHERLANDS
UM GEO-OCEAN
IN WOS Cotutelle UMR
   copubli-france
   copubli-europe
   copubli-univ-france
IF 3.6
TC 4
UR https://archimer.ifremer.fr/doc/00761/87335/94781.pdf
LA English
DT Article
DE ;reef coastal defense;wave dissipation;wave setup;wave runup;field measurements;XBeach model simulations
AB Coral reefs represent an efficient natural mechanical coastal defense against ocean waves. The focus of this study is La Saline fringing coral reef, located in the microtidal West of La Réunion Island in the Indian Ocean, frequently exposed to Southern Ocean swell and cyclonic events. The aim is to provide a better understanding of the reef's coastal defense characteristics for several Southern Ocean swell events. Pressure sensors were placed across the reef to measure water level fluctuations and to study wave transformation. A numerical model (XBeach surfbeat), validated using field observations, was used to deepen understanding of wave transformation, wave setup and runup. Field measurements and model outputs show that as gravity waves dissipate over the reef, and frequency-dependent dissipation of infragravity waves by bottom-friction occurs, the reef acts as a low-pass filter. Wave-induced setup is found to be the dominant hydrodynamic component. Setup and runup are each 98% and 79% driven by the offshore significant wave height, and 2% and 21% driven by the tide. The modulation of the water level by setup is the main contributor to runup in the fringing reef. At semidiurnal timescales, setup and runup are in antiphase with tidal variations as lower water levels result in higher gravity wave energy dissipation, setup and runup. Simple-to-use transfer functions relating incident wave characteristics to these hydrodynamic components are proposed. The effects of bottom friction and water level on the defensive capacity of the coral reef highlight future implications of structural damage and sea level rise. Key Points Study of wave transformation over La Saline fringing reef, a natural coastal defense against Southern Ocean swell and cyclonic events As gravity waves dissipate over the fringing reef, significant energy transfer to infragravity and very low frequency bands occurs Wave setup and runup are greater for higher offshore wave height (HS0) and lower water level. Modeled runup scales as ≈20% of HS0 Plain Language Summary Coral reefs protect the coastline from ocean waves. The protective characteristics of reefs are site-dependent as they vary according to a number of parameters such as coral health, water depth, oceanic and meteorological conditions. La Saline fringing reef on La Reunion Island is frequently exposed to Southern Ocean swell and cyclonic events. Accompanied by numerical modeling efforts, pressure sensors placed across the reef allow to study water level fluctuations for a range of swell events and tides. Results show that waves transform as they break and dissipate over the reef, as the energy of higher-frequency waves is transferred toward lower frequencies. At the study site, offshore significant wave height is the main driver of the reef hydrodynamics. The tide also contributes by modulating the water level over the reef flat. In the context of predicted sea level rise in recent climate change scenarios, as well as possible reef health decline, present study results suggest that the protective capacity of the La Saline fringing reef could decline, thus altering future reef hydrodynamics and associated sediment transport. 
PY 2022
PD JUN
SO Journal Of Geophysical Research-oceans
SN 2169-9275
PU American Geophysical Union
VL 127
IS 7
UT 000822734700001
DI 10.1029/2022JC018570
ID 87335
ER

EF