FN Archimer Export Format
PT J
TI Tide and wave driven flow across the rim reef of the atoll of Raroia (Tuamotu, French Polynesia)
BT 
AF Aucan, Jerome
   DESCLAUX, Terence
   Le Gendre, Romain
   Liao, Vetea
   Andréfouët, Serge
AS 1:1;2:2;3:2;4:3;5:1;
FF 1:;2:PDG-RBE-LEADNC;3:PDG-RBE-LEADNC;4:;5:;
C1 Institut de Recherche Pour le Développement (IRD), UMR 9220 ENTROPIE (Institut de Recherche Pour le Développement, Université de la Réunion, IFREMER, Université de la Nouvelle-Calédonie, Centre National de la Recherche Scientifique), Nouméa, New Caledonia
   Institut Français de Recherche pour l'Exploitation de la MER, UMR 9220 ENTROPIE (Institut de Recherche Pour le Développement, Université de la Réunion, IFREMER, Université de la Nouvelle-Calédonie, Centre National de la Recherche Scientifique), Nouméa, New Caledonia
   Marine Resources Division, Government of French Polynesia, French Polynesia
C2 IRD, FRANCE
   IFREMER, FRANCE
   MARINE RESOURCES DIV, FRANCE
SI NOUMEA
SE PDG-RBE-LEADNC
UM ENTROPIE
IN WOS Ifremer UMR
   WOS Cotutelle UMR
   copubli-france
   copubli-p187
IF 7.001
TC 8
UR https://archimer.ifremer.fr/doc/00705/81690/86749.pdf
LA English
DT Article
CR MALIS
   MALIS 2018
BO Alis
DE ;Pearl farming;Lagoon;Coral reef;Hydrodynamic
AB The currents flowing across the rim of the atoll of Raroia were investigated with a 1 year-long dataset of wave, water level and currents. Offshore waves break on the edge of the reef outside the atoll's rim and drive current into the lagoon, through the shallow hoa that cut across the rim. The additional water volume generated by this wave driven flow induces an elevation of water level throughout the atoll's lagoon and is evacuated back into the open ocean through a deep reef pass. The water level inside the atoll is also driven by astronomical tides, which enter the lagoon thought the reef pass, after undergoing a ~50% decrease in amplitude and a ~4 hour lag. Using a simple parametric model with three calibrated coefficients, we show that currents across the atoll's rim can be estimated as a function of the offshore wave conditions and the water level difference between the ocean and the lagoon. 
PY 2021
PD OCT
SO Marine Pollution Bulletin
SN 0025-326X
PU Elsevier BV
VL 171
UT 000701706200004
DI 10.1016/j.marpolbul.2021.112718
ID 81690
ER

EF