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At the present time, little is known about how broad salinity and temperature ranges are for seawater thermodynamic models that are functions of absolute salinity (S A ), temperature (T ) and pressure (P ). Such models rely on fixed compositional ratios of the major components (e.g. Na/Cl, Mg/Cl, Ca/Cl, SO 4 /Cl, etc.). As seawater evaporates 5doi:10.5194/osd-6-171-2009 fatcat:uzhqxkprwrcvholvhp6lq5aaku