Geography and ecology of the Everglades is nourished primarily from the atmosphere. Before the first attempt at draining the Everglades in 1882, the entire watershed extended from Orlando to Florida Bay comprising the Kissimmee–Lake Okeechobee–Everglades (KLOE) watershed. Kissimmee River outlets flow into Lake Okeechobee, which sits above sea level. Only two seasons exist in the Everglades: wet (May to November) and dry (December to April). Average annual rainfall in the Everglades is approximately , though fluctuations of precipitation are normal. Droughts, floods, and tropical storms are normal occurrences in the area. When Lake Okeechobee exceeds its water storage capacity during the wet season, it pours slowly
Okeechobee Plain Okeechobee Plain The Okeechobee Plain is a major geologic feature of Florida formed during the Pliocene and Pleistocene epochs and named for Okeechobee County, Florida, United States. The Okeechobee Plain is a dry prairie or grassland The Okeechobee Plain is within the Kissimmee/Okeechobee Lowland established by the Florida Department of Environmental Protection's Lake Bioassessment/Regionalization Initiative. The Okeechobee Plain was created during the Pliocene and Pleistocene's wild climatic times through continuous depositing of sediments from rivers as the peninsula grew southward. During the Piacenzian (3.6—2.5 Ma) stage of the Pliocene the plain, was, for the most part, submerged and is referred