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Question: use the linear equation of state of seawater to calculate...

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Use the linear equation of state of seawater to calculate the density of freshwater (0 salinity) and ocean water (35 salinity) at 15C and zero pressure (relative to sea level pressure). Next look up the water properties for North Atlantic Deep Water and Antarctic Bottom Water. Use representative temperature and salinity values for each water mass to calculate the densities at zero pressure. Which water mass is denser? Does it make sense that Antarctic Bottom Water found below the North Atlantic Deep Water? How does the density difference between water masses compare to the difference between completely fresh and salty water from the first part of this problem?

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