HB1105 ReadMe Class of Data: Surface ocean carbon dioxide concentrations Dataset Identifier: HB1105-Legs 1-5 Autumn Bottom Trawl Survey Expocode: 33HH20110909 Statement of how to cite dataset: Bigelow website: http://www.aoml.noaa.gov/ocd/gcc/rvbigelow_introduction.php For more information on dataset citation please see Master Readme File. Measurement platform identifier: NOAA Ship Henry B. Bigelow, R225 Time period the dataset refers to: 9 Sept, 2011 - 15 Nov, 2011 Geographic area the dataset refers to: Latitude, 34.4 to 44.7 degree north Longitude, 65.7 to 76.0 degree west Standard and Reference Gases: The four CO2 standard cylinders come from Scott-Marrin, Inc., and are calibrated with primary standards that are directly traceable to the WMO scale. The zero gas is ultra-high purity air. Any value outside the range of the standards should be considered approximate (+/-5 ppm). While individual data points above 520 or below 200 may less accurate, the general trends would be indicative of the seawater chemistry. The standards used on the cruise are: STANDARD TANK # [CO2]ppm VENDOR STD1 JA02645 204.74 Scott-Marrin STD2 JA02273 317.49 Scott-Marrin STD3 JA02285 372.23 Scott-Marrin STD4 JA02647 518.24 Scott-Marrin STD5 JA03093 0.00 Scott-Marrin Data quality issues: The LICOR analyzer was serviced on 8 October, between legs 2 and 3 of HB1105. To ensure consistancy, the data for legs 1 and 2 were processed together and the data for legs 3 through 5 were processed together. The files containing the 15-second averages of the ship's underway sensors were used to fill gaps in the data appended to the CO2 data in real-time (new values: 3273 barometric pressures, 3104 sea surface temperatures, 3081 salinities). After the merging of CO2 data with the data files of ship's sensors, there remained three gaps of more than ten analyses without important supporting data. From 15:04 to 15:27 on 27 Sept and from 14:23 to 14:48 on 28 Sept, the missing data were barometric pressure, SST, and salinity. A value of 32 psu was assigned as the salinity. From 04:36 to 05:58 on 28 Sept, SST and salinity were missing. A value of 33 psu was assigned as the salinity. For the fifty analyses before and after each relavant gap, the average difference between the LICOR and barometric pressures was 0.12 (+/- 0.18) mbar and the average difference between the equilibrator temperature and SST was 0.25 (+/- 0.24) degree centrigrade. For these gaps, the barometric pressure was estimated by adding 0.12 to the LICOR pressure and the SST was estimated by subtracting 0.25 from the equlibrator temperature. Timestamp for dataset reduction: 22 Nov, 2011 Timestamp for most recent update of dataset: 22 Nov, 2011 Matlab version used for reduction: 1.10 Contact person for this dataset: Kevin Sullivan (305)361-4382 Kevin.Sullivan@noaa.gov