gsw_brineSA_CT
Absolute Salinity of seawater at the freezing point
Contents
USAGE:
brineSA_t = gsw_brineSA_t(t,p,saturation_fraction)
DESCRIPTION:
Calculates the Absolute Salinity of seawater at the freezing temperature.
That is, the output is the Absolute Salinity of seawater, with the
fraction saturation_fraction of dissolved air, that is in equilibrium
with ice at in-situ temperature t and pressure p. If the input
values are such that there is no positive value of Absolute Salinity for
which seawater is frozen, the output, brineSA_t, is put equal to -99.
INPUT:
t = in-situ temperature (ITS-90) [ deg C ]
p = sea pressure [ dbar ]
( i.e. absolute pressure - 10.1325 dbar )
OPTIONAL:
saturation_fraction = the saturation fraction of dissolved air in
seawater.
( i.e., saturation_fraction must be between 0 and 1, and the default
is 1, completely saturated )
p & saturation_fraction (if provided) may have dimensions 1x1 or Mx1 or
1xN or MxN, where t is MxN.
OUTPUT:
brineSA_t = Absolute Salinity of seawater when it freezes, for
given input values of in-situ temperature
pressure and air saturation fraction. [ g/kg ]
EXAMPLE:
t = [-0.11901; -0.15608; -0.72138; -1.97738; -2.31728; -2.56764;]
p = [ 10; 50; 125; 250; 600; 1000;]
saturation_fraction = 1
brineSA_t = gsw_brineSA_t(t,p,saturation_fraction)
brineSA_t =
2.017072489768256
2.151989342038463
11.677649626115610
32.843128114999026
34.136459306273444
33.097427522625168
AUTHOR:
Trevor McDougall and Paul Barker [ help@teos-10.org ]
VERSION NUMBER:
3.01 (16th May, 2011)
REFERENCES:
IOC, SCOR and IAPSO, 2010: The international thermodynamic equation of
seawater - 2010: Calculation and use of thermodynamic properties.
Intergovernmental Oceanographic Commission, Manuals and Guides No. 56,
UNESCO (English), 196 pp. Available from the TEOS-10 web site.
See section 3.3 of this TEOS-10 Manual.
The software is available from http://www.TEOS-10.org