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Atchafalaya Basin. The wetlands of Louisiana are water-saturated coastal and swamp regions of southern Louisiana, often called "Bayou".. The Louisiana coastal zone stretches from the border of Texas to the Mississippi line [1] and comprises two wetland-dominated ecosystems, the Deltaic Plain of the Mississippi River (unit 1, 2, and 3) and the closely linked Chenier Plain (unit 4). [2]
The conservation area borders the entire north shore area of White Lake, with a diverse habitat, is self-sustaining, and managed by the Louisiana Department of Wildlife and Fisheries (LDWF). There are approximately 53,249 acres of freshwater marsh and 18,656 acres of leased property that includes croplands, wetlands, wooded areas, and campsites.
Louisiana Wildlife Management Areas are protected conservation areas within the state of Louisiana. The goal is protecting, conserving, and replenishing wildlife, including all aquatic life. The goal is protecting, conserving, and replenishing wildlife, including all aquatic life.
Similarly to the rest of Louisiana, the Sound experiences a semitropical climate. [1] The average water temperatures range from 70˚F to 84˚F (21–29°C) by month and the humidity ranges between 73% and 84%. Due to the humidity, clouds often form overhead, reducing the amount of daily sunlight that the area receives to as little as 4 hours. [2]
Summers in southern Louisiana have high temperatures from June through September averaging 90 °F (32 °C) or more, and overnight lows averaging above 70 °F (21 °C). At times, temperatures in the 90s °F (32–37 °C), combined with dew points in the upper 70s °F (24–26 °C), create sensible temperatures over 120 °F (49 °C). The humid ...
It was drained by the Old River, French Fork and a number of bayous until several flood control projects changed the lake's drainage characteristics. It is known as the largest moist soil unit in North America and supports a variety of waterfowl including geese , duck , and wading birds and is a recreational area for hunting, fishing, hiking ...
This decrease in flow across the floodplain, in conjunction with high organic deposition from trees and floating vegetation and high water temperature, has resulted in large areas of low-dissolved oxygen water. Where once the water was black (1850), the water became brown (1927). Where the water was formerly brown (1927), it is now black (2009 ...
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