QC for Hydrographic Data GEOSECS to GO-SHIP. Susan M. Becker Scripps Institution of Oceanography Oceanographic Data Facility

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QC for Hydrographic Data GEOSECS to GO-SHIP Susan M. Becker Scripps Institution of Oceanography Oceanographic Data Facility

Global Hydrographic Efforts Geo-chemical Ocean Sections (GEOSECS) World Ocean Circulation Experiment (WOCE) Joint Global Ocean Flux Studies (JGOFS) Climate and Ocean Variability (CLIVAR) Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP) http://www.go-ship.org/hydroman.html

GO-SHIP STANDARDS FOR CTD SENSORS Temperature Accuracy = 0.002 C. Precision = 0.0005 C (ITS90). Salinity Accuracy = 0.002 g kg-1 (TEOS-10) depending on frequency and technique of calibration. Precision = 0.001 g kg-1 (TEOS-10), depending on processing techniques. Pressure Accuracy = 3 decibar (dbar) with careful laboratory calibration. Precision = 0.5 dbar, dependent on processing. O2 Accuracy = 1%. Same for precision.

STS calibration of Pressure Sensors Pressure laboratory calibrations are done at several temperatures to provide coefficients that are corrected for the effect of temperature at sea: Follow the recommendations in the GO-SHIP methods: monitor on-deck pressure values at the beginning and end of every cast, and from cast to cast. Usually no additional adjustment is necessary, and on-deck pressure stays within 1 dbar of pre-cruise calibrations

At Sea Calibration of CTD Sensors Temperature calibrations: comparison of primary and secondary SBE 3plus temperatures on each cast a single SBE 35 at bottle stops as a tertiary temperature check. Two independent metrics of conductivity correction accuracy are examined: At each bottle closure, the primary and secondary conductivity are compared with each other. Each sensor is also compared to conductivity calculated from check sample salinities using CTD pressure and temperature. Collecting and calibrating electrochemical oxygen sensor profiles of dissolved oceanic oxygen data requires some expertise and perhaps some art as well. When calibrations are complete, the residuals between oxygen sensor data and bottle oxygen sample data should be small (< 2 μmol kg-1 overall and even < 1 μmol kg-1 in some locations of the water column) if water sample data quality are high and oxygen sensor performance is good.

GO-SHIP STANDARDS FOR WATER SAMPLES Salinity: Accuracy of 0.001 is possible with Autosal salinometers O2: Target accuracy is that 2 sigma should be less than 0.5% of the highest concentration found in the ocean. Precision or reproducibility (2 sigma) is 0.08% of the highest concentration found in the ocean NO3 approximately 1% accuracy and 0.2% precision, full scale PO4 approximately 1-2% accuracy and 0.4% precision, full scale SiO2 approximately 1-3% accuracy and 0.2% precision, full scale

P06

P06

SIO RMNS Summary For NO3 and PO4, the observed differences between the deep data and the differences between the observed RMNS values and the assigned values are within the intra cruise variability (<1%) The intra cruise variability for SIL was good (<1%) For SIL the observed differences data is very close to the observed difference in the observed vs. assigned RMNS values

Summary The potential changes scientists are looking for are at or near the detection limits of most sensors and instruments. It is critical that any observed changes are not due to differences in sensors, methodologies, or differences in calibration standards, laboratories collecting and analyzing the data for the different ocean parameters. Purkey and Johnson (2010, 2012) CARINA (Carbon In the Atlantic) [Key et al., 2010] GLODAP (GLobal Ocean Data Analysis Project) [Key et a., 2004] GLODAP V2 Hood, E.M., C.L. Sabine, and B.M. Sloyan, eds. 2010. The GO-SHIP Repeat Hydrography Manual: A Collection of Expert Reports and Guidelines. IOCCP Report Number 14, ICPO Publication Series Number 134. Available online at http://www.go-ship.org/hydroman.html.