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Atmospheric instability is a condition where the Earth's atmosphere is considered to be unstable and as a result local weather is highly variable through distance and time. [ clarification needed ] [ 1 ] Atmospheric instability encourages vertical motion, which is directly correlated to different types of weather systems and their severity.
There are a number of environmental issues in Florida.A large portion of Florida is a biologically diverse ecosystem, with large wetlands in the Everglades.Management of environmental issues related to the everglades and the larger coastal waters and wetlands have been important to the history of Florida and the development of multiple parts of the economy of Florida, including the influential ...
Stable stratification of fluids occurs when each layer is less dense than the one below it. Unstable stratification is when each layer is denser than the one below it. Buoyancy forces tend to preserve stable stratification; the higher layers float on the lower ones. In unstable stratification, on the other hand, buoyancy forces cause convection ...
A 5,000 mile-long blob of slimy, smelly seaweed is headed for Florida’s beaches on the Gulf of Mexico, and it’s partly because of human activity, including water pollution and climate change.
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A storm surge inundation map released at 11 a.m. by the NHC shows the potential for more than 9 feet of water flooding into vulnerable Tampa Bay, Charlotte Harbor, and Fort Myers Beach.
Brevard County has 8,000 miles (13,000 km) of waterline, presenting a challenge to water environmental management. In 2013, there were four major problems with water quality in the Indian River Lagoon. 1) Excess nitrogen and phosphorus from runoff from the application of fertilizer; 2) an estimated 8 to 11% septic tank failure. There are tens ...
Unstable areas are in yellow (slightly) and red (highly) while the stable zone is in blue. The lifted index ( LI ) is the temperature difference between the environment Te(p) and an air parcel lifted adiabatically Tp(p) at a given pressure height in the troposphere (lowest layer where most weather occurs) of the atmosphere , usually 500 hPa ( mb ).