gsw_internal_energy_first_derivatives

SA, CT and p partial derivatives of internal_energy
(75-term equation)

Contents

USAGE:

[u_SA, u_CT, u_P] = gsw_internal_energy_first_derivatives(SA,CT,p)

DESCRIPTION:

Calculates the three (3) partial derivatives of internal energy with 
respect to Absolute Salinity, Conservative Temperature and pressure.  
Note that the pressure derivative is done with respect to pressure in 
Pa, not dbar.  This function uses the computationally-efficient 75-term
expression for specific volume in terms of SA, CT and p (Roquet et al.,
2015).
Note that the 75-term equation has been fitted in a restricted range of 
parameter space, and is most accurate inside the "oceanographic funnel" 
described in McDougall et al. (2003).  The GSW library function 
"gsw_infunnel(SA,CT,p)" is avaialble to be used if one wants to test if 
some of one's data lies outside this "funnel". 

INPUT:

SA  =  Absolute Salinity                                        [ g/kg ]
CT  =  Conservative Temperature                                [ deg C ]
p   =  sea pressure                                             [ dbar ]
       (ie. absolute pressure - 10.1325 dbar)
SA & CT need to have the same dimensions.
p may have dimensions 1x1 or Mx1 or 1xN or MxN, where SA & CT are MxN.

OUTPUT:

u_SA  =  partial derivative of internal_energy with respect to     
             Absolute Salinity          [ (J/kg)(g/kg)^-1 ] i.e. [ J/g ]
u_CT  =  partial derivative of internal_energy with respect to           
             Conservative Temperature                    [ (J/kg) K^-1 ]
u_P   =  partial derivative of internal energy with respect to          
             pressure in Pa                             [ (J/kg) Pa^-1 ]

EXAMPLE:

SA = [34.7118; 34.8915; 35.0256; 34.8472; 34.7366; 34.7324;]
CT = [28.8099; 28.4392; 22.7862; 10.2262;  6.8272;  4.3236;]
p =  [     10;      50;     125;     250;     600;    1000;]
[u_SA, u_CT, u_P] = gsw_internal_energy_first_derivatives(SA,CT,p)
u_SA =
   0.071187610402307
   0.071215557423953
   0.071105286125378
   0.069730589312430
   0.049035910573059
   0.002958348659863
u_CT =
   1.0e+03 *
   3.991835761856051
   3.991835867574300
   3.991839270596763
   3.991844970098064
   3.991815048606444
   3.991738836685656
u_P =
   1.0e-03 *
   0.978707891379082
   0.978464186284615
   0.976704798645003
   0.974063899959057
   0.973627094487500
   0.973297052143081

AUTHOR:

Paul Barker and Trevor McDougall          [ help@teos-10.org ]

VERSION NUMBER:

3.05 (16th February, 2015)

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., D.R. Jackett, D.G. Wright and R. Feistel, 2003: 
 Accurate and computationally efficient algorithms for potential 
 temperature and density of seawater.  J. Atmosph. Ocean. Tech., 20,
 pp. 730-741.
Roquet, F., G. Madec, T.J. McDougall, P.M. Barker, 2015: Accurate
 polynomial expressions for the density and specifc volume of seawater
 using the TEOS-10 standard. Ocean Modelling.
The software is available from http://www.TEOS-10.org