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- W48051231 abstract "Fringing reefs have been described as being morphologicallysimple (Kennedy and Woodroffe, 2002), but variation in important parameters such as the reef morphology, tidalrange, and wave energy means that a widely applicablemodel of fringing reef water circulation does not exist. Fundamental distinctions can be made between fringing reefswith or without an enclosed lagoon, those on the windwardshores (with circulation normally driven by waves) or leeward shores (with tidal and other currents dominating),and those enclosed by headlands (where topographicallycontrolled circulation is important) or those that extendalong a more or less straight shoreline. Other reef types that could be described as fringing are variously described as either fringing or barrier (e.g., Ningaloo Reef, Australia; Hearn, 1999), bank-fringing (e.g., Great Pond Bay, St Croix, U.S. Virgin Islands; Lugo-Fernandez et al., 1998b), bank-barrier (e.g., Tague Reef, St Croix; Lugo-Fernandez et al., 2004), or coral lagoons (e.g., Kaneohe Bay, Oahu, Hawaii; Hearn, 1999). Other authors have described reefs adjacent to coral cays as fringing (Daly and Brander, 2006)." @default.
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- W48051231 date "2011-01-01" @default.
- W48051231 modified "2023-09-24" @default.
- W48051231 title "Fringing reef circulation" @default.
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