
|
The map above on the left illustrates average simulated predrainage surface water ponding depths and overland flow patterns. The hydroperiod map above on the right shows the average number of days during a typical year that the region was inundated. The levees and canals of the current system did not exist circa 1850, and they are shown for geographic reference only. The pre-drainage system was characterized by a broad spatial extent of surface water which persisted over a large area. The slow moving 50-mile wide, 100-mile long "river of grass" extended from Lake Okeechobee to Florida Bay and the Gulf of Mexico. As a precursor to ecological restoration of the Everglades, current efforts are focused on enhancing the hydrologic characteristics of the remaining Everglades to more closely mimic those of the predrainage Everglades system. Achieving hydrologic restoration does not guarantee ecological restoration; however it is assumed that reconstructing the natural or pre-drained hydrologic characteristics will provide maximum opportunity for recovery of the remaining Everglades landscape patterns and Everglades wildlife.
1Source: SFWMD Hydrologic Systems Modeling Division. Natural System Model (NSM) Version 4.5. The NSM simulates the hydrologic response of the pre-drainage Everglades system to historical (1965-95) meteorologic data.
|
|||||
|
U.S. Department of the Interior, U.S. Geological Survey, Center for Coastal Geology This page is: http://sofia.usgs.gov/sfrsf/rooms/hydrology/water/wherebefore.html Contact: webmaster@sflwww.er.usgs.gov Last updated: 11 October, 2002 @ 09:42 PM (HSH) |