There are different kinds of process that deeply affects the salinity of ocean water. Continental deflections, Coriolis Effect, convection current and also evaporation.
The three factors that form deep ocean currents are temperature, salinity, and density. These factors influence the movement of water masses in the ocean, creating currents that can circulate for thousands of kilometers.
Oceanographers can determine ocean currents, density variations, and the distribution of marine organisms by using the temperature and salinity of ocean water. These properties influence the movement of water masses and the distribution of marine life in different parts of the ocean.
A river flowing into the sea is causing the decrease in salinity
Biomass and temperature, erosion and mineral content.
Yes, temperature, salinity, and density are all factors in the formation of ocean currents. These factors affect the movement of water masses, which can create differences in water density and drive the circulation of ocean currents. Changes in temperature and salinity can impact the density of water, influencing the speed and direction of currents.
salinity
You could increase the salinity of the ocean by adding salt or removing water (ie: by evaporation).
The lowest areas of salinity in an ocean are near where fresh water rivers empty into them. This is because the influx of fresh water creates an area of lower salinity compared to the remainder of the ocean.
Storms at sea. The evaporated water falls back into the ocean with no net effect on salinity.
By using information about the temperature and salinity of ocean water oceangraphers can describe the?
The density of the water increases with the salinity, so saline water is denser and sinks to the bottom. Temperature is also a factor, however. Cold, saline water is the densest