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Partial pressure of carbon dioxide, temperature, salinity and other variables collected from the coastal surface underway observations from NOAA Ship Henry B. Bigelow in the North Atlantic Ocean, US North-East coast in 2019 (NCEI Accession 0191370)

INVESTIGATORS:
Rik Wanninkhof ORCID logo - NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML)
Denis Pierrot ORCID logo - NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML)
Kevin F. Sullivan - NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML)

PACKAGE DESCRIPTION: This dataset includes surface underway, chemical, meteorological and physical data collected from NOAA Ship Henry B. Bigelow in the North Atlantic Ocean, US North East coast from 2019-03-08 to 2019-11-12. These data include measurements of mole fraction of carbon dioxide (CO2) in the equilibrator headspace (dry) at equilibrator temperature, mole fraction of CO2 measured in dry outside air, barometric pressure in the equilibrator headspace, barometric pressure, corrected to sea level, water temperature in equilibrator, sea surface temperature, sea surface salinity, fugacity of CO2 in sea water at SST and 100% humidity, and difference between sea water fugacity of CO2 (fCO2) and interpolated air fCO2. The instruments used to collect these data include carbon dioxide gas analyzer and shower head chamber equilibrator for autonomous carbon dioxide measurement. In February 2011, the Ocean Carbon Group at NOAA's Atlantic Oceanographic and Meteorological Laboratory (AOML) installed an instrument to measure CO2 levels in surface water and air on NOAA Ship Henry B. Bigelow. The Bigelow primarily operates in the North Atlantic Ocean between North Carolina and Maine.

CITE AS: Wanninkhof, Rik; Pierrot, Denis; Sullivan, Kevin F. (2019). Partial pressure of carbon dioxide, temperature, salinity and other variables collected from the coastal surface underway observations from NOAA Ship Henry B. Bigelow in the North Atlantic Ocean, US North-East coast in 2019 (NCEI Accession 0191370). [indicate subset used]. NOAA National Centers for Environmental Information. Dataset. https://doi.org/10.25921/fypj-t662. Accessed [date].


DATA PACKAGES RELATED TO THIS ONE:
IDENTIFICATION INFORMATION FOR THIS DATA PACKAGE:
NCEI ACCESSION: 0191370
NCEI DOI: https://doi.org/10.25921/fypj-t662
EXPOCODE: 33HH20190308; 33HH20190326; 33HH20190411; 33HH20190501; 33HH20190522; 33HH20190614; 33HH20190725; 33HH20190819; 33HH20190903; 33HH20190925; 33HH20191012; 33HH20191030;
CRUISE ID: HB1901_Legs1-4 Spring Bottom Trawl Survey; HB1902 Spring NE EcoMon; HB1903 NE Deep Water Corals Habitats; HB1904 Mesopelagic Exploration Deepsea; HB1905 Bottom Trawl Gear Research; HB1906_Legs1-4 Autumn Bottom Trawl Survey;
SECTION/LEG: Coastal;

TYPES OF STUDY:
Coastal;Surface underway;

TEMPORAL COVERAGE:
START DATE: 2019-03-08
END DATE: 2019-11-12

SPATIAL COVERAGE:
NORTH: 44.56
WEST: -76.11
EAST: -65.35
SOUTH: 34.49

GEOGRAPHIC NAMES:
North Atlantic Ocean;

PLATFORMS:
NOAA Ship Henry B. Bigelow (ID: 33HH);

RESEARCH PROJECT(S):
NOAA Ocean Acidification Program (OAP);


VARIABLES / PARAMETERS:

pCO2 (fCO2) autonomous
Abbreviation: fCO2_SW@SST
Unit: uatm
Observation type: Surface underway
Measured or calculated: Measured
Sampling instrument: Seawater pump
Location of seawater intake: Bow
Analyzing instrument: Infrared Analyzer: LI-COR model 6262
Detailed sampling and analyzing information: Pierrot, D., Neill, C., Sullivan, K., Castle, R., Wanninkhof, R., Lüger, H., Johannessen, T., Olsen, A., Feely, R. A., & Cosca, C. E. (2009). Recommendations for autonomous underway pCO2 measuring systems and data-reduction routines. Deep Sea Research Part II: Topical Studies in Oceanography, 56(8-10), 512-522. https://doi.org/10.1016/j.dsr2.2008.12.005
Equilibrator type: Spray head above dynamic pool, with thermal jacket
Equilibrator volume: 0.95 L (0.4 L water, 0.55 L headspace)
Is the equilibrator vented or not: Vented
Water flow rate: 1.5 - 2.0 L/min
Gas flow rate: 70 - 150 ml/min
How was temperature inside the equilibrator measured: Hart Scientific model 1523 digital thermometer
How was pressure inside the equilibrator measured: External Setra 270 connected to the exit of the analyzer
Drying method for gas: Gas stream passes through a thermoelectric condenser (~5 C) and then through a Perma Pure (Nafion) dryer before reaching the analyzer (90% dry).
SEA CO2 gas detector manufacturer: Licor, Inc
SEA CO2 gas detector model: Licor 6262
SEA CO2 gas detector resolution: 0.01 uatm
SEA CO2 gas detector uncertainty: 2 uatm
Standardization technique: The analyzer is calibrated every 4.3 hours with field standards that in turn were calibrated with primary standards that are directly traceable to the WMO scale. The zero gas is ultra-high purity air.
Standardization frequency: Every 4.3 hours
Standard gas manufacturer: Scott-Marrin, Inc.
Standard gas concentration: Std 1: JA02166, 232.80 ppm, owned by AOML, used every ~4.5 hours. Std 2: JB03651, 306.46 ppm, owned by AOML, used every ~4.5 hours. Std 3: JB03592, 422.24 ppm, owned by AOML, used every ~4.5 hours. Std 4: JB03285, 565.58 ppm, owned by AOML, used every ~4.5 hours. Std 5: LL100000, 0.00 ppm, owned by AOML, used every ~23.5 hours.
Standard gas uncertainty: 0.01 ppm
Water vapor correction method: Details of the data reduction are described in Pierrot, et.al. (2009).
Temperature correction method: Details of the data reduction are described in Pierrot, et.al. (2009).
At what temperature was pCO2 reported: In situ sea surface temperature
Uncertainty: 0.01C
Quality flag convention: WOCE quality control flags are used: 2 = good value, 3 = questionable value, 4 = bad value
Method reference: Pierrot, D., Neill, C., Sullivan, K., Castle, R., Wanninkhof, R., Lüger, H., Johannessen, T., Olsen, A., Feely, R. A., & Cosca, C. E. (2009). Recommendations for autonomous underway pCO2 measuring systems and data-reduction routines. Deep Sea Research Part II: Topical Studies in Oceanography, 56(8-10), 512-522. https://doi.org/10.1016/j.dsr2.2008.12.005
Researcher name: Kevin Sullivan
Researcher institution: NOAA/AOML
Sea Surface Temperature
Abbreviation: SST_C
Unit: degrees celcius
Observation type: Surface Underway
Analyzing instrument: SBE 38, Seabird, Inc.
Detailed sampling and analyzing information: After sea water pump, ~3 m below sea surface
Uncertainty: Accuracy: 0.001C, Precision: 0.0003C
Researcher name: Kevin Sullivan
Researcher institution: NOAA/AOML
Sea Surface Salinity
Abbreviation: SAL_permil
Observation type: Surface Underway
Analyzing instrument: SBE 45, Seabird, Inc.
Uncertainty: Accuracy: +/- 0.005; Precision: 0.0002
Researcher name: Kevin Sullivan
Researcher institution: NOAA/AOML
Atmospheric Pressure
Abbreviation: PRES_ATM@SSP_hPa
Unit: hPa
Analyzing instrument: Vaisala, Model: PTB220
Uncertainty: Accuracy: +/- 0.15 hPa; Precision: 0.01 hPa
Researcher name: Kevin Sullivan
Researcher institution: NOAA/AOML

PUBLICATIONS DESCRIBING THIS DATASET:
Pierrot, D., Neill, C., Sullivan, K., Castle, R., Wanninkhof, R., Lüger, H., Johannessen, T., Olsen, A., Feely, R. A., & Cosca, C. E. (2009). Recommendations for autonomous underway pCO2 measuring systems and data-reduction routines. Deep Sea Research Part II: Topical Studies in Oceanography, 56(8-10), 512-522. https://doi.org/10.1016/j.dsr2.2008.12.005
ADDITIONAL INFORMATION:
none;
FUNDING AGENCY:
NOAA Climate Program Office Program
PROJECT TITLE: NOAA Ocean Acidification Program
PROJECT ID:

SUBMITTED BY: Kevin F. Sullivan (Kevin.Sullivan@noaa.gov)

SUBMISSION DATE: 2019-07-11

REVISION DATE: 2019-12-04

PREVIOUS VERSIONS: Version 1.1Version 2.2