latent heat of evaporation
CT = gsw_latentheat_evap_CT(SA,p,)
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.
SA = Absolute Salinity [ g/kg ]
CT = Conservative Temperature [ deg C ]
SA & CT need to have the same dimensions.
latentheat_evap_CT = latent heat of evaporation [ J/kg ]
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)
Paul Barker, Trevor McDougall and Rainer Feistal [ email@example.com ]
3.05 (16th February, 2015)
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