gsw_adiabatic_lapse_rate_ice

Contents

USAGE:

adiabatic_lapse_rate_ice = gsw_adiabatic_lapse_rate_ice(t,p)

DESCRIPTION:

Calculates the adiabatic lapse rate of ice from in-situ
temperature.

INPUT:

t  =  in-situ temperature (ITS-90)                             [ deg C ]
p  =  sea pressure                                              [ dbar ]
      (ie. absolute pressure - 10.1325 dbar)

p may have dimensions 1x1 or Mx1 or 1xN or MxN, where t is MxN.

OUTPUT:

adiabatic_lapse_rate_ice  =  adiabatic lapse rate of ice        [ K/Pa ]
  Note.  The output is in unit of degress Celsius per Pa,
    (or equivilently K/Pa) not in units of K/dbar.

EXAMPLE:

t = [-10.7856; -13.4329; -12.8103; -12.2600; -10.8863; -8.4036;]
p = [      10;       50;      125;      250;      600;    1000;]

adiabatic_lapse_rate_ice = gsw_adiabatic_lapse_rate_ice(t,p)

adiabatic_lapse_rate_ice =

  1.0e-007 *

   0.218777853913651
   0.216559115188599
   0.216867659957613
   0.216988337914416
   0.217182707402780
   0.218100558740840

AUTHOR:

Trevor McDougall and Paul Barker                    [ 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.

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