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Cape San Blas was home to a Confederate saltworks where 150 US bushels (5.3 m 3) of salt a day were processed by evaporation of seawater. This halted in 1862, when a landing party from the Union ship, the USS Kingfisher, destroyed the saltworks. Cape San Blas has had four lighthouses. The first, built in 1847, collapsed during a gale on August ...
The first Cape San Blas Light was completed in 1849 with an appropriation of $8,000 made 2 years earlier. The shoals running out from the cape extended 3.5 or 4.3 nautical miles; 6.4 or 8.0 kilometres (4 or 5 mi) and made it dangerous for all vessels nearing the coast.
August 15 – Tropical Storm Fred – Fred reached its peak intensity as a strong tropical storm with winds of 65 mph (105 km/h) at 18:00 UTC on August 16 shortly before making landfall a few miles southeast of Mexico Beach near Cape San Blas, Florida at a similar intensity around an hour later at 19:15 UTC. [196] [197]
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CAPE was estimated to exceed 8 kJ/kg in the environment of the Plainfield storm and was around 7 kJ/kg for the Jarrell storm. Severe weather and tornadoes can develop in an area of low CAPE values. The surprise severe weather event that occurred in Illinois and Indiana on April 20, 2004, is a good example. Importantly in that case, was that ...
The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats. It varies depending on depth, geographical location and season. Not only does the temperature differ in seawater, so does the salinity. Warm surface water is generally saltier than the cooler deep or polar waters. [1]
At 18:00 UTC on August 16, Fred peaked with winds of 65 mph (105 km/h) and a minimum pressure of 993 mbar (29.3 inHg), just over an hour before making landfall near Cape San Blas, Florida. Fred weakened to a tropical depression over Alabama on August 17, before weakening into a remnant low over Tennessee at 00:00 UTC on August 18.
Charts of sea surface temperature in and near False Bay in summer and winter. In summer False Bay is thermally stratified, with a vertical temperature variation of 5 to 9˚C between the warmer surface water and cooler depths below 50 m, while in winter the water column is at nearly constant temperature at all depths.