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Many physical processes over ocean surface generate sea salt aerosols. One common cause is the bursting of air bubbles, which are entrained by the wind stress during the whitecap formation. Another is tearing of drops from wave tops. [19] The total sea salt flux from the ocean to the atmosphere is about 3300 Tg (3.3 billion tonnes) per year. [20]
Cyclic salt is salt that is carried by the wind when it comes in contact with breaking waves. It is estimated that more than 300 million tons of cyclic salt is deposited on the Earth 's surface each year, and it is considered to be a significant factor in the chlorine content of the Earth's river water.
The San Francisco Bay Salt Ponds are a roughly 16,500-acre (6,700 ha) part of the San Francisco Bay that have been used as salt evaporation ponds since the California Gold Rush era. Most of the ponds were once wetlands in the cities of Redwood City , Newark , and Hayward , and other parts of the bay.
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This is a list of bodies of water by salinity that is limited to natural bodies of water that have a stable salinity above 0.05%, at or below which water is considered fresh.
Lemoore (formerly, La Tache and Lee Moore's) [5] is a city in Kings County, California, United States. Lemoore is located 7.5 miles (12 km) west-southwest of Hanford , [ 8 ] at an elevation of 230 feet (70 m). [ 5 ]
Computer models of ocean circulation increasingly place most of the deep upwelling in the Southern Ocean, associated with the strong winds in the open latitudes between South America and Antarctica. [28] Direct estimates of the strength of the thermohaline circulation have also been made at 26.5°N in the North Atlantic, by the UK-US RAPID ...
The salt can come from one of two processes: the dissolution of large salt deposits through salt tectonics [2] or geothermally-heated brine issued from tectonic spreading centers. [ 3 ] The brine often contains high concentrations of hydrogen sulfide and methane , which provide energy to chemosynthetic organisms that live near the pool.