O2ptoO2c.m

function O2conc=O2ptoO2c(pO2,T,S,P)
%function O2conc=O2ptoO2c(pO2,T,S,P)
%
% convert oxygen partial pressure to molar oxygen concentration
%
% inputs:
%   pO2    - oxygen partial pressure in mbar
%   T      - temperature in °C
%   S      - salinity (PSS-78)
%   P      - hydrostatic pressure in dbar (default: 0 dbar)
%
% output:
%   O2conc - oxygen concentration in umol L-1
%
% according to recommendations by SCOR WG 142 "Quality Control Procedures
% for Oxygen and Other Biogeochemical Sensors on Floats and Gliders"
%
% Henry Bittig
% Laboratoire d'Océanographie de Villefranche-sur-Mer, France
% bittig@obs-vlfr.fr
% 28.10.2015
% 19.04.2018, v1.1, fixed typo in B2 exponent

% set input default
if nargin<4, P     = 0;       end

xO2     = 0.20946; % mole fraction of O2 in dry air (Glueckauf 1951)
pH2Osat = 1013.25.*(exp(24.4543-(67.4509*(100./(T+273.15)))-(4.8489*log(((273.15+T)./100)))-0.000544.*S)); % saturated water vapor in mbar
sca_T   = log((298.15-T)./(273.15+T)); % scaled temperature for use in TCorr and SCorr
TCorr   = 44.6596.*exp(2.00907+3.22014.*sca_T+4.05010.*sca_T.^2+4.94457.*sca_T.^3-2.56847e-1.*sca_T.^4+3.88767.*sca_T.^5); % temperature correction part from Garcia and Gordon (1992), Benson and Krause (1984) refit mL(STP) L-1; and conversion from mL(STP) L-1 to umol L-1
Scorr   = exp(S.*(-6.24523e-3-7.37614e-3.*sca_T-1.03410e-2.*sca_T.^2-8.17083e-3.*sca_T.^3)-4.88682e-7.*S.^2); % salinity correction part from Garcia and Gordon (1992), Benson and Krause (1984) refit ml(STP) L-1
Vm      = 0.317; % molar volume of O2 in m3 mol-1 Pa dbar-1 (Enns et al. 1965)
R       = 8.314; % universal gas constant in J mol-1 K-1

O2conc=pO2./(xO2.*(1013.25-pH2Osat)).*(TCorr.*Scorr)./exp(Vm.*P./(R.*(T+273.15)));