The salinity of ocean water depends on its location, rate of evaporation, amount of precipitation and amount of freshwater added to the ocean.
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The main reasons for higher salt content in surface ocean water are evaporation and formation of sea ice. As water evaporates, salt is left behind, causing an increase in salinity. In regions where sea ice forms, the salt is expelled, further increasing the salinity of the remaining water.
Yes the estuarities in salinity make it increase high. The carbon dioxide makes the ocean water decrease.
Yes, it is possible for a volcano to lie beneath the surface of the ocean. These are known as submarine volcanoes or seamounts. When they erupt, they can create new underwater landforms and contribute to the formation of underwater mountain ranges.
Upwelled water is cooler, nutrient-rich, and has higher concentrations of dissolved gases compared to the surrounding water. This is because upwelling brings nutrient-rich water from deeper ocean layers up to the surface, supporting higher productivity in marine ecosystems.
Evaporation occur at the surface of the ocean.
Surface water slainity is higher in tropical regions.
Deep ocean currents and surface currents do interact and influence each other. While they flow at different depths and have different driving factors (wind for surface currents and density for deep currents), they are connected through the global ocean circulation system. Changes in one can impact the other over time.