oce (version 0.1-76)

sw.S.C.T.p: Seawater salinity from conductivity ratio, temperature and pressure

Description

Compute salinity, given conductivity ratio, temperature, and pressure.

Usage

sw.S.C.T.p(C, t, p)

Arguments

C

conductivity ratio [unitless]

t

in-situ temperature [$^\circ$C]

p

pressure [dbar]

Value

• Salinity [PSU].

Details

Calculate S from what is actually measured by the CTD, i.e. the conductivity ratio C, the in-situ temperature T, and the pressure p. Often this is done by the CTD processing software, but sometimes it is helpful to do this directly, e.g. when there is a concern about mismatches in sensor response times. S is calculated using the UNESCO algorithm described by Fofonoff and Millard (1983).

References

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

See Also

sw.conductivity

Examples

print(sw.S.C.T.p(1,15,2000))   # 34.25045
print(sw.S.C.T.p(1.2,20,2000)) # 37.24563
print(sw.S.C.T.p(0.65,5,1500)) # 27.99535