“…Mean spring tide is mainly diurnal, ranging from 0.6 to 0.8 m (Harris, 1981;NOAA, 1985a;Forbes, 1988). Dominant nearshore currents are to the west (Beall, 1968;Becker, 1972;USACE, 1974;Crout and Hamiter, 1981;NOAA, 1985b) and are controlled by winds and waves that are predominantly from the southeast (USACE, 1974;Hubbertz and Brooks, 1989). Gammill (2002) provides a detailed review of historical water levels and their impact on marsh evolution throughout the Chenier Plain.…”