//0
//UTF-8
//File updated on 11/11/2025 15:39
//!! ADJUSTED DATA FILE !!
//WMO ID: 5904479
//Institution ID: 0276
//MBARI ID: un0276
//Project Name: UW
//Region: NAtl
//Missing Float profile(s) for station(s): 127 143 152 162 163 164 165 166 167 168 169 170 171 172 173 174 175 176 179 180 181 182 183 184 185 186 187 188 189 190 191 192 193
//No position for station(s): 195 196 197
//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 5595
//Temperature[°C] Sbe41cp 5595
//Salinity[pss] Sbe41cp 5595
//Sigma_theta[kg/m^3] Potential density at the sea surface
//Depth[m] Depth calculated from pressure and latitude
//Oxygen[µmol/kg] SBE63J 455
//OxygenSat[%] Calculation assumes atmospheric pressure= 1013.25 mbar
//Nitrate[µmol/kg] SUNA 0348
//Chl_a[mg/m^3] MCOMS 0014 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 0014 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 0014 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 0014
//
//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 >