The astronomical high tide line was compiled from National Wetlands
Inventory (NWI) 1:24,000-scale habitat maps that were photo-interpreted from
color-infrared aerial photography acquired between November 1988 and March
1989 at a scale of 1:65,000. Inland extent of tidal influence was then
determined from the 1988 Chabreck and Linscombe marsh vegetation maps,
photo-interpretation, field review, and information gathered from
discussions with regional and local experts. Only semi-diurnal and diurnal
gravity tides are considered in the NWI classification because of the
general lack of information on wind-influenced tidal fluctuations and
ranges. All saltwater wetlands (saline, brackish, and intermediate) in
coastal Louisiana were considered to be tidal unless impounded, and tidally
influenced freshwater wetlands were included in the tidal zone as well. In
general, the division between salt water and fresh water is considered to be
the limit of gravitation tidal influence for coastal Louisiana.
Arcs that close delineate isolated areas above the astronomical
high tide line, but are not built into topological polygons.