Enter temperature and salinity to find density σ_{t}.

Enter temperature, salinity and pressure to find *in-situ* density σ_{Stp}.

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.
Add 1000 to the result to obtain density in kg m 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 Sciences 44, 53 pp.

© 2000 M. Tomczak. Last updated 2 April 2000