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Salinity

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Salinity
The mentioned graph, (figure 9.4), shows variations in the ocean’s surface temperature as well as the salinity as the position of latitude changes. Salinity is a measurement of how much salt concentration that can be found in the ocean water. It affects characteristics of water quality and has a tremendous impact where plant and animal life can flourish. The degree of salinity directly relates with surface temperatures in the ocean. In areas where there are higher temperatures, there will be a large amount of evaporation. As a result, the salinity of the ocean water will be higher. Additionally, rainfall is another factor which will affect ocean salinity (Lutgens, Tarbuck, & Tasa, 2011).
If I were to explain this in layman’s terms, I would rationalize this solution in the following way. If I used a 50 gallon drum and filled it with 30 gallons of water and added 1 pound of salt, this mixture would have a 30 to 1 ratio of water to salt. If I then left the filled drum in 100º F of direct sunlight for one week, a portion of the water in the drum will have evaporated and the degree of salt in the solution would be higher. However, if I were to do the same experiment for a one week period with cooler days, and added 10 gallons of water to the drum, the salinity of the solution would be less.
Additionally, other influences from nature such as rivers, volcanoes, and select types of animal and plant life assist in keeping the water at consistent salinity levels. This would indicate that the overall levels of salt in sea water remain unchanged. As a result, the water which is at the equator most likely has decreased salinity due to the high amount of rainfall which affects the volume of water. This would also play a key role in the lack of evaporation due to cloud cover preventing the sun’s direct light and heat from evaporating large amounts of seawater (Talley,

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