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Measuring the density of seawater can be achieved using accepted equations of state if certain parameters are known. This article includes links to the equations.
There is also a discussion of how mismatches in sensor response times (primarily between conductivity and temperature) cause anomalous errors in the salinity data (spiking). |
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Measuring the salinity of seawater can be achieved using accepted equations of state if certain parameters are known. This article includes links to the equations.
There is also a discussion of how mismatches in sensor response times (primarily between conductivity and temperature) cause anomalous errors in the salinity data (spiking).
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