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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]
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 ...
Much of the Gulf Coast has a summer precipitation maximum, with July or August commonly the wettest month due to the combination of frequent summer thunderstorms produced by relentless heat and humidity, and tropical weather systems, including tropical depressions, tropical storms, and hurricanes, while winter and early spring rainfall also can ...
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 ...
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.
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Typically, salinity is higher along the eastern shore, near Pass Manchac. Due to Lake Maurepas’s shallow depth, even relatively low energy wave action results in sediment resuspension and, therefore, relatively high turbidity and low transparency, which influences the degree to which primary production can occur in the water column and ...