HIGHLIGHTS
SUMMARY
Presently, many fundamental oceanographic variables such as the density of seawater, the sea level anomaly and the geostrophic velocity are calculated or modeled employing the thermodynamic equation of seawater of 2010 (TEOS-10, IOC et_al, 2010). The reference composition of seawater has been defined by Millero et_al, 2008. It should be noted, however, that in Lago et_al, 2015, made laboratory measurements of c in the range (273.15 to 313.15) K and in the absolute salinity range (10.036 to Frontiers in Marine Science Instruments to measure speed of sound To date, the . . .
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