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P16N

  • Nitrate (SIO)
  • Phosphate (SIO)
  • Silicate (SIO)
  • Oxygen (SIO)
  • TCO2 (Feely - PMEL) - +4 µmol/kg correction recommended.
  • Crossovers:
    Crossing # old # Latitude Longitude Cruise 1 Cruise 1 Sta Cruise 2 Cruise 2 Sta Delta Stdev
    47 17 53° N 152° W P16N 58,59,66 P17N 78 -9.0 5.1
    49   30° N 152° W P16N 30,31,32 P2 70 -7.6 3.0
    MEAN -8.3 1.0
  • Precision of Duplicate Measurements - No Information.
  • CRM Results - CRM batch was bad. Precision 1.2-3 µmol/kg.
  • Multiparameter Analysis (details) - Mean Difference (estimated - measured) = 3.1 ± 4.1
  • Isopycnal Analysis - Results of our isopycnal analysis of P2 and P16N TCO2 near 30° N, 152° W indicates consistently higher TCO2 values (8-10 µmol/kg) in deep water on the P2 line as compared with P16N (Figure). The P14 data along 179° W also show slightly higher deep water values (mean = 4 µmol/kg) than the P16N results. In the previous crossover and MLR analyses P14 showed no obvious offsets, whereas the P2 were generally found to be high and the P16N data were consistently low. The results of the isopycnal analysis can be reconciled with the findings of the other methods if the P16N data are increased by ~4 µmol/kg and the P2 data are decreased by 4-6 µmol/kg.
  • Alkalinity - (Not Measured)
  • fCO2 - (Not Measured)
  • pH (Byrne - USF) - We recommend adjusting all spectrophotometric pH values upward by 0.0047 to be internally consistent with the other carbon parameters.
Last modified: 2021-03-17T18:30:27Z