//0
//UTF-8
//File updated on 11/04/2025 08:55
//!! ADJUSTED DATA FILE !!
//WMO ID: 5904847
//Institution ID: 0689
//MBARI ID: un0689
//Project Name: SOCCOM
//Region: SO
//No missing float profiles
//Missing Float position interpolated for station(s): 21 22 23 24 25 26 27 28 29 30 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 94 95 96 97 98 99 100 101 102 103 104 105 106 107 134 135 136 137 138 139 140 141 142
//Latitude quality flag = 4 for interpolated float positions
//No missing data found
//"IceEvRec" = 1 indicates that the float was unable to surface as a result of the ice-avoidance algorithm. Note that this result does not necessarily signify the presence of sea-ice.
//"IceEvRec" = 0 indicates that the float was able to surface as a result of the ice-avoidance algorithm (and/or the absence of ice-avoidance algorithm software, ie for low-latitude floats)
//For more information on the technical aspects of the ice-avoidance algorithm onboard profiling floats, please see Riser et al (2018) https://doi.org/10.1002/2017JC013419
//label="IceEvRec" value_type="INTEGER" significant_digits="0"
//
//FLOAT VARIABLES:
//Variable Sensor Serial number Comment
//Pressure[dbar] Sbe41cp 8485
//Temperature[°C] Sbe41cp 8485
//Salinity[pss] Sbe41cp 8485
//Sigma_theta[kg/m^3] Potential density at the sea surface
//Depth[m] Depth calculated from pressure and latitude
//Oxygen[µmol/kg] SBE63 1372
//OxygenSat[%] Calculation assumes atmospheric pressure= 1013.25 mbar
//Nitrate[µmol/kg] SUNA 0815
//Chl_a[mg/m^3] MCOMS 0129 See: Boss, E.B. and N. Haëntjens, 2016. http://soccom.princeton.edu/sites/default/files/files/SOCCOM_2016-1_Bio-optics-primer.pdf
//b_bp700[1/m] MCOMS 0129 See: Boss, E.B. and N. Haëntjens, 2016. http://soccom.princeton.edu/sites/default/files/files/SOCCOM_2016-1_Bio-optics-primer.pdf
//POC[mmol/m^3] MCOMS 0129 See: Boss, E.B. and N. Haëntjens, 2016. http://soccom.princeton.edu/sites/default/files/files/SOCCOM_2016-1_Bio-optics-primer.pdf
//pHinsitu[Total] SBE C15
//pH25C[Total] SBE C15 estimated with CO2SYS(TALK_LIAR,pHinsitu) for Matlab see note below
//TALK_LIAR[µmol/kg] TALK_LIAR = Alkalinity estimated with the LIAR V2.2 algorithim Eqn7, MeasIDVec = [1 6 7] (PSAL, DOXY_ADJ, TEMP), (Carter et al., 2016,doi:10.1002/lom3.10087; Carter et al., 2017, https://doi.org/10.1002/lom3.10232).LIAR code used was downloaded on 10/31/2018 from https://github.com/BRCScienceProducts/LIRs.
//DIC_LIAR[µmol/kg] estimated with CO2SYS(TALK_LIAR,pHinsitu) for Matlab (see note below)
//pCO2_LIAR[µatm] estimated with CO2SYS(TALK_LIAR,biased pHinsitu) for Matlab (see note below)
//CDOM[ppb] MCOMS 0129
//
//NOTE ON CO2SYS CARBONATE SYSTEM CALCULATIONS:
//All carbonate system variables calculated with CO2SYS for Matlab
//(Sharp et al., 2020; see also Lewis and Wallace 1998)
//used the following conditions: pH was reported on the total scale.
//K1 and K2 dissociation constants were from Lueker et al., 2000, doi:
//10.1016/S0304-4203(00)00022-0. The KSO4 dissociation constant was
//from Dickson, 1990, doi: 10.1016/0021-9614(90)90074-Z. The KF dissociation
//constant was from Perez and Fraga 1987, doi: 10.1016/0304-4203(87)90036-3.
//The borate to salinity ratio was from Lee et al., 2010,
//doi:10.1016/j.gca.2009.12.027. Silicate and Phosphate were not
//measured by the float, but estimates based on Redfieldian ratios improved
//the carbonate system estimates. If a nitrate value was considered to
//be of good quality silicate = nitrate*2.5 and phosphate = nitrate/16,
//otherwise the best estimate for both was considered to be 0. When pCO2
//was estimated from TALK_LIAR and pHinsitu, a bias was first added to pHinsitu
//following Williams et al., 2017, doi: https://doi.org/10.1002/2016GB005541 , section 3.4, equation 3.
//This correction is not necessary for DIC and DIC is computed with the reported pH and the TALK_LIAR value.
//
//NOTE ON Chl_a [mg/m^3] CONCENTRATION:
//There is community-established calibration bias of 2 for the WET Labs 413 ECO-series fluorometers
//(Roesler et al, 2017, doi: 10.1002/lom3.10185).
//Chl_a has been recalculated using in situ measured dark counts. Chl_a is then divided by the Roesler factor of 2.
//Lastly, profiles with sun elevaltion >