Three processes that control salinity are evaporation, precipitation, and freshwater inflow. Evaporation increases salinity as water vapor leaves the surface, concentrating the dissolved salts in the remaining water. Precipitation decreases salinity by adding freshwater, which dilutes the concentration of salts in the water. Freshwater inflow from rivers or melting ice also reduces salinity by introducing lower-salinity water into saltier bodies, balancing the overall salinity levels.
Oceans are big water bodies. Salinity is due to the presence of minerals in water.
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Surface salinity in polar regions varies seasonally due to the formation and melting of sea ice.
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The salinity of water in polar regions varies seasonally because of the melting of sea ice during warmer months.
During warmer months the salinity level goes down because of ice melting. Ice is mostly fresh water.
Coastal waters have a lower salinity due to the vast amount of freshwater runoff pouring into the sea from rivers and streams. PM
Three factors are evaporation and freezing of sea water.
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Scientists explain changes in the Earth through processes such as plate tectonics, erosion, volcanic activity, and climate change. These changes are often driven by natural phenomena and Earth's dynamic systems over geological time scales. By studying evidence from rocks, fossils, and other data, scientists can better understand the forces shaping the Earth's geology and environment.
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