# gsw_latentheat_evap_CT

    latent heat of evaporation

## Contents

- USAGE:
- DESCRIPTION:
- INPUT:
- OUTPUT:
- EXAMPLE:
- AUTHOR:
- VERSION NUMBER:
- REFERENCES:

## 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.

    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              [ deg C ]

## 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:

    3.02 (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.
      See section 3.3 of this TEOS-10 Manual.

    The software is available from http://www.TEOS-10.org