AndreaBozzo/ceres-open-data-index huggingface dataset:
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R4 (Hobart-Dumont d'Urville station)

This data was collected in February 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R4.

Departed:  Hobart, Australia, February 19, 2013
Arrived:  	 Dumont d'Urville station, Antarctica, February 25, 2013


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R4 (Dumont d'Urville station - Hobart)

This data was collected in February - March 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R4.

Departed:   Dumont d'Urville station, Antarctica, February 26, 2013
Arrived:  Hobart Australia, March 04, 2013


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R2 (Hobart-Dumont d'Urville station)

This data was collected in January 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R2.

Departed:  Hobart, Australia, January 10, 2013
Arrived:  	 Dumont d'Urville station, Antarctica, January 15, 2013


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R2 (Dumont d'Urville station - Hobart)

This data was collected in January 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R2.

Departed:   Dumont d'Urville station, Antarctica, January 26, 2012
Arrived:  Hobart Australia, January 31, 2012


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R0 (Hobart-Dumont d'Urville station)

This data was collected in October 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R0.

Departed:  Hobart, Australia, October 23, 2012
Arrived:  	 Dumont d'Urville station, Antarctica, October 28, 2012


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Macquarie Island, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1213R0 (Dumont d'Urville station - Hobart)

This data was collected in November 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1213R0.

Departed:   Dumont d'Urville station, Antarctica, November 17, 2012
Arrived:  Hobart Australia, November 22, 2012


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1112R4 (Hobart-Dumont d'Urville station)

This data was collected in February 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1112R4.

Departed:  Hobart Australia, February 19, 2012
Arrived:  	 Dumont d'Urville station, Antarctica, February 25, 2012


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1112R4 (Dumont d'Urville station - Hobart)

This data was collected in March 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1112R4.

Departed:   Dumont d'Urville station, Antarctica, March 02, 2012
Arrived:  Hobart Australia, March 07, 2012


CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from MV L'Astrolabe voyage AL1112R2 (Hobart-Dumont d'Urville station)

This data was collected in January 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on MV L'Astrolabe (IMOS platform code: FHZI) voyage AL1112R2.

Departed:  Hobart Australia, January 06, 2012
Arrived:  	 Dumont d'Urville station, Antarctica, January, 2012

Data was collected from 7th-12th of January.

CO2 System Overview:
The fugacity of carbon dioxide (fCO2) in surface seawater was measured using a General Oceanics Inc. automated system (Model 8050; Pierrot et al 2009). Seawater is sprayed into an equilibration chamber and CO2 in the headspace gas equilibrates with the seawater. The headspace gas is pumped through a thermoelectric condenser followed by a nafion drying tube, before flowing through a Licor 7000 non-dispersive infrared gas analyser used to measure the CO2 mole fraction (XCO2) of the dried air. The gas flow is stopped temporarily for the CO2 measurements, which are made at atmospheric pressure. A set of four CO2 standards (Table 1) that cover the range of CO2 values expected in the ocean are analysed about every three hours to calibrate the gas analyser. Atmospheric XCO2 (dry) is measured after the standards by pumping clean outside air from an intake on the forward mast of the ship. 

The seawater intake is at about 3m depth in the bow of the ship. A remote temperature sensor (Seabird Electronics SBE38) located at the intake is used to measure sea surface temperature (SST). Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) mounted in the bow thruster space near the intake. The travel time between the intake and CO2 system is typically about 50 seconds with warming usually less than 0.4ºC. The thermosalinograph water is from the same intake and supply line. Meteorological data, salinity, SST, and ships position and time are taken from the ship’s logging system. The salinity values measured by the SBE21 were checked against discrete bottle samples collected on the voyage.

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system.

Tags: Antarctica, Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Continents, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart