south florida everglades historically: free-flowing ‘river of grass’ extending from the...
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South Florida Everglades
• Historically: Free-flowing ‘river of grass’ extending from the Kissimmee chain of lakes to Florida Bay.
• Since late 1800s: Construction of 3,000 km of canals and levees inter-rupting the Everglades' natural sheetflow, eliminating more than 50% of the wetlands and deterioration of water quality.SeaWiFS: April 1999
Annual precipitation (smoothing average), horizontal line = historic average.Richardson 2010
• Plant communities highly influenced by rainfall patterns combined with impact of drainage, dikes, and an occasional hurricane.
• Timing, frequency and amplitude of low and high water events.
• Shifts in rainfall also control nutrient loadings.
Historic map of the plant communities in the Everglades based on the map of J.H. Davis (1943). The map has been redrawn and simplified from the original map, and the boundaries of the current water conservation areas (WCA-1,WCA-2, WCA-3), the Everglades National Park (ENP), and the Everglades Agricultural Areas have been added (form Richardson 2010)
Shallow elevation gradient and overlying peat storage of water during wet periods and slow release during dry season.
Richardson 2010
Everglades Restoration
Plan• Restoration of natural
hydrological conditions• Restoration of wetland habitat
and biological populations• Improved water quality• Enhanced water supply for
agriculture and urban use• Continued flood protection• Cost: $7.8 billion (now $11
billion)• Duration: 30 years
Richardson 2010
Succession patterns related to fire and hydroperiod in the Everglades. Modified from Richardson 2000
The current Everglades ecosystem is not simply rainfall driven.It depends on the restoration of peatland hydrology and nutrient
conditions.
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