//0
//UTF-8
//File updated on 11/05/2025 09:27
//!! ADJUSTED DATA FILE !!
//WMO ID: 5904475
//Institution ID: 0037
//MBARI ID: un0037
//Project Name: SOCCOM
//Region: SO
//Missing Float profile(s) for station(s): 69 70 71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 87 118 220
//No position for station(s): 224
//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 9895
//Temperature[°C] Sbe41cp 9895
//Salinity[pss] Sbe41cp 9895
//Sigma_theta[kg/m^3] Potential density at the sea surface
//Depth[m] Depth calculated from pressure and latitude
//Oxygen[µmol/kg] SBE63J 0449
//OxygenSat[%] Calculation assumes atmospheric pressure= 1013.25 mbar
//Nitrate[µmol/kg] SUNA 0171
//Chl_a[mg/m^3] MCOMS 0015 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 0015 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 0015 See: Boss, E.B. and N. Haëntjens, 2016. http://soccom.princeton.edu/sites/default/files/files/SOCCOM_2016-1_Bio-optics-primer.pdf
//CDOM[ppb] MCOMS 0015
//
//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 >