gsw_latentheat_evap_CT

latent heat of evaporation

Contents

USAGE:

CT = gsw_latentheat_evap_CT(SA,p,)

DESCRIPTION:

Calculates latent heat of evaporation of water from seawater 
(isobaric evaporation enthalpy) with CT as input temperature at p = 0 (the 
surface).  It is defined as a function of Absolute Salinity, SA, and
Conservative Temperature, CT, and is valid in the ranges 
0 < SA < 42 g/kg and 0 < CT < 40 deg C.  The errors range between 
-0.4 and 0.6 J/kg.
TEOS-10 
Click for a more detailed description of calculating
latent heat of evaporation.

INPUT:

SA  =  Absolute Salinity                                        [ g/kg ]
CT  =  Conservative Temperature                                [ deg C ]
SA & CT need to have the same dimensions.

OUTPUT:

latentheat_evap_CT  =  latent heat of evaporation               [ J/kg ]

EXAMPLE:

SA = [34.7118; 34.8915; 35.0256; 34.8472; 34.7366; 34.7324;]
CT = [28.7856; 28.4329; 22.8103; 10.2600;  6.8863;  4.4036;]
latentheat_evap_CT = gsw_latentheat_evap_CT(SA,CT)
latentheat_evap_CT =
  1.0e+006 *
   2.429947107462561
   2.430774073049213
   2.444220372158452
   2.474127109232524
   2.482151446148560
   2.488052297193594

AUTHOR:

Paul Barker, Trevor McDougall and Rainer Feistal    [ 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.
  See section 3.3 of this TEOS-10 Manual.
The software is available from http://www.TEOS-10.org