Contents
USAGE:
z = gsw_z_from_p(p,lat,{geo_strf_dyn_height})
DESCRIPTION:
Calculates height from sea pressure using the computationally-efficient
48-term expression for density in terms of SA, CT and p. (McDougall et
al., 2013).
Note. Height z is NEGATIVE in the ocean. ie. Depth is -z.
Depth is not used in the GSW computer software library.
INPUT:
p = sea pressure [ dbar ]
( ie. absolute pressure - 10.1325 dbar )
OPTIONAL:
geo_strf_dyn_height = dynamic height [ m2/s^2 ]
lat = latitude in decimal degrees north [ -90 ... +90 ]
lat may have dimensions 1x1 or Mx1 or 1xN or MxN, where p is MxN.
OUTPUT:
z = height [ m ]
Note. At sea level z = 0, and since z (HEIGHT) is defined to be
positive upwards, it follows that while z is positive in the
atmosphere, it is NEGATIVE in the ocean.
EXAMPLE:
p = [ 10; 50; 125; 250; 600; 1000;]
lat = 4;
z = gsw_z_from_p(p,lat)
z =
1.0e+002 *
-0.099445831334188
-0.497180888338818
-1.242726230109135
-2.484700703230813
-5.958254446096435
-9.920921779551200
AUTHOR:
Trevor McDougall, Claire Roberts-Thomson & Paul Barker.
[ help@teos-10.org ]
VERSION NUMBER:
3.02 (17th November, 2012)
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.
McDougall T.J., P.M. Barker, R. Feistel and D.R. Jackett, 2013: A
computationally efficient 48-term expression for the density of
seawater in terms of Conservative Temperature, and related properties
of seawater. To be submitted to J. Atm. Ocean. Technol., xx, yyy-zzz.
Moritz (2000) Goedetic reference system 1980. J. Geodesy, 74, 128-133.
This software is available from http://www.TEOS-10.org