gsw_SAAR
Absolute Salinity Anomaly Ratio
Contents
USAGE:
SAAR = gsw_SAAR(p,long,lat)
DESCRIPTION:
Calculates the Absolute Salinity Anomaly Ratio.
INPUT:
p = sea pressure [ dbar ]
( i.e. absolute pressure - 10.1325 dbar )
long = longitude in decimal degrees [ 0 ... +360 ]
or [ -180 ... +180 ]
lat = latitude in decimal degrees north [ -90 ... +90 ]
p, long & lat need to have the same dimensions.
OUTPUT:
SAAR = Absolute Salinity Anomaly Ratio [ unitless ]
in_ocean = 0, if long and lat are a long way from the ocean
= 1, if long and lat are in the ocean
Note. This flag is only set when the observation is well and truly on
dry land; often the warning flag is not set until one is several
hundred kilometres inland from the coast.
EXAMPLE:
p = [ 10; 50; 125; 250; 600; 1000;]
lat = [ 4; 4; 4; 4; 4; 4;]
long = [ 188; 188; 188; 188; 188; 188;]
[SAAR, in_ocean] = gsw_SAAR(p,long,lat)
SAAR =
1.0e-003 *
0.004794295602143
0.007668755837570
0.018919828449091
0.077293264028981
0.161974583039298
0.270652408428964
in_ocean =
1
1
1
1
1
1
AUTHOR:
Paul Barker and Trevor McDougall [ help@teos-10.org ]
VERSION NUMBER:
3.01 (23rd 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 http://www.TEOS-10.org
See section 2.5 of this TEOS-10 Manual.
McDougall, T.J., D.R. Jackett and F.J. Millero, 2010: An algorithm
for estimating Absolute Salinity in the global ocean. Submitted to
Ocean Science. A preliminary version is available at Ocean Sci. Discuss.,
6, 215-242.
http://www.ocean-sci-discuss.net/6/215/2009/osd-6-215-2009-print.pdf
The software is available from http://www.TEOS-10.org