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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]
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Use of the term "cyclic" refers to the cycle in which the salt moves from sea to land and is then washed by rainwater back to the sea. The salt (and other solid matter) cannot evaporate as water does. Instead it leaves the ocean surface in fine droplets of drop impacts or bubble bursts. Wave-crests and other turbulence form foam.
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 ...
Although the amount of salt in the ocean remains relatively constant within the scale of millions of years, various factors affect the salinity of a body of water. [27] Evaporation and by-product of ice formation (known as "brine rejection") increase salinity, whereas precipitation , sea ice melt, and runoff from land reduce it. [ 27 ]
The restaurant's exterior, 2022. Drew Tyson included Ocean City in Thrillist's 2014 "guide to Portland's 6 best dim sum spots". He wrote, "One of the big three on 82nd and a well-known haven for Asian food, Ocean City might not get the general recognition of Wong's King... but if you ask most of the city's top chefs they'd say this spot is their favorite.
Salt Shack on the Bay is a seafood restaurant in Tampa, Florida. [1] Established in July 2019, the business was included in The New York Times 's 2023 list of the 50 best restaurants in the United States.
The Arctic Ocean has historically ranged from roughly 14-16 million square kilometers in late winter to roughly 7 million km 2 each September. [6] The annual increase of ice plays a major role in the movement of ocean circulation and deep water formation. The density of the water below the newly-formed ice increases due to brine rejection.