Note: 10 kPa = 1 dbar is close to the pressure increase that corresponds to a depth increase of 1 m.
Entering a pressure value equal to the depth in metres will give an approximate result. Temperature uses IPTS-68, salinity uses PSS-78; see reference. |
Calculation based on Fofonoff, P. and R. C. Millard Jr (1983) Algorithms for computation of fundamental properties of seawater. Unesco Technical Papers in Marine Science 44, 53 pp.
Note: This calculator determines salinity from measurements of in situ conductivity (as obtained, for example, while lowering a CTD). The quantity used in the determination of salinity in bench salinometers is the conductivity ratio Rt(S,t) = C(S,t,0) / (C,35,t,0) where S is salinity, t is temperature and C is conductivity. To determine salinity from this salinity ratio, use the salinity from conductivity ratio calculator. |
© 2000 M. Tomczak. Last updated 22 August 2000
contact address: