//0
//UTF-8
//File updated on 11/15/2025 12:24
//!! ADJUSTED DATA FILE !!
//WMO ID: 2903863
//Institution ID: 0063
//MBARI ID: un0063
//Project Name: GO-BGC
//Region: NPac
//No missing float profiles
//Missing Float position interpolated for station(s): 164
//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 18944
//Temperature[°C] Sbe41cp 18944
//Salinity[pss] Sbe41cp 18944
//Sigma_theta[kg/m^3] Potential density at the sea surface
//Depth[m] Depth calculated from pressure and latitude
//Oxygen[µmol/kg] SBE83 0089
//OxygenSat[%] Calculation assumes atmospheric pressure= 1013.25 mbar
//Nitrate[µmol/kg] SUNA 2073
//Chl_a[mg/m^3] MCOMS 433 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 433 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 433 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 12387
//pH25C[Total] SBE 12387 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 433
//DOWN_IRRAD380[W/m^2/nm] OCR504 2347
//DOWN_IRRAD412[W/m^2/nm] OCR504 2347
//DOWN_IRRAD490[W/m^2/nm] OCR504 2347
//DOWNWELL_PAR[µmol Quanta/m^2/sec] OCR504 2347
//
//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 >