AndreaBozzo/ceres-open-data-index huggingface dataset:
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1213VMS (Hobart-Hobart)

This data was collected in September - November 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1213VMS.

Departed: 	Hobart, Tasmania, September 14, 2012
Arrived:  Hobart, Tasmania,  November 16, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1213V4 (Hobart-Hobart)

This data was collected in February - March 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1213V4.

Departed: 	Hobart, Tasmania, February 28, 2013
Arrived:  Hobart, Tasmania,  March 14, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1213V3 (Hobart-Hobart)

This data was collected in January - February 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1213V3.

Departed: 	Hobart, Tasmania, January 13, 2013
Arrived:  Hobart, Tasmania,  February 22, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP-XBT Upper Ocean Thermal Data collected during a cruise between Sydney and Noumea (New Caledonia)

This dataset contains temperature data obtained from XBTs (expendable bathythermographs) deployed during a cruise between Sydney and Noumea (New Caledonia).

Tags: Australia, Bathythermographs, Bluewater and Climate, Countries, Expendable Bathythermographs, IMOS Node, IMOS Sub-Facility, New Caledonia, Ocean Pressure, Ocean Temperature, Oceans, Pacific Ocean, Regional Seas, SOOP-XBT, Tasman Sea, Water Pressure, Water Temperature
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1213V2 (Hobart-Hobart)

This data was collected in December 2012 - January 2013 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1213V2.

Departed: 	Hobart, Tasmania, December 20, 2012
Arrived:  Hobart, Tasmania,  January 08, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1213V1 (Hobart-Hobart)

This data was collected in November - December 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1213V1.

Departed: 	Hobart, Tasmania, November 19, 2012
Arrived:  Hobart, Tasmania,  December 14, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1112V6 (Hobart-Hobart)

This data was collected in April/May2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1112V5.

Departed: 	Hobart, Tasmania,  April 16, 2012
Arrived:  Hobart, Tasmania,  May 01, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1112V4 (Fremantle-Hobart)

This data was collected in February/March 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1112V4.

Departed: 	Fremantle, Western Australia,  February 15, 2012
Arrived:  Hobart, Tasmania,  March 15, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, Western Australia, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP-XBT Upper Ocean Thermal Data collected on the line PX2 (across the Banda Sea)

Temperature data from the TOGA/WOCE transect PX2 across the Banda Sea (Flores Sea - Torres Strait) has been collected since 1983 and are ongoing. The transect is repeated approximately 12 times a year with profiles obtained approximately every 50-100 Km. 
The data are obtained from XBTs (expendable bathythermographs) deployed vie marchant vessels, and are managed by the Joint Australian Facility for Ocean Observing Systems (JAFOOS), a collaborative venture between CSIRO Marine Research and the Bureau of Meteorology Research Centre (BMRC).

Tags: Australia, Banda Sea, Bathythermographs, Bluewater and Climate, Countries, Expendable Bathythermographs, Flores Sea, IMOS Node, IMOS Sub-Facility, Ocean Pressure, Ocean Temperature, Oceans, Regional Seas, SOOP-XBT, Water Pressure, Water Temperature
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1112V3 (Hobart-Fremantle)

This data was collected in January/February 2012 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1112V3.

Departed: 	Hobart, Tasmania,  January 05, 2012
Arrived:  Fremantle, Western Australia,  February 12, 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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, Western Australia, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA1112V1 (Hobart-Hobart)

This data was collected in July/August 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1112V1.

Departed: 	Hobart, Tasmania,  July 19, 2011
Arrived:  Hobart, Tasmania,  August 05, 2011

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 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. 

Seawater intake and ancillary data:
The seawater intake is at about 6 m depth. 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 oceanographic lab next to the pCO2 system. The travel time between the intake and CO2 system is typically about 70 seconds with warming usually less than 0.7ºC in cold waters near freezing. 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.

Tags: Atmosphere, Atmospheric Pressure, Australia, Australian Antarctic, Bluewater and Climate, Carbon Dioxide Measurements, Countries, IMOS Node, IMOS Sub-Facility, Multidisplinary Underway Network, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, SOOP-CO2, Salinity, Sea Surface Temperature, Southern Ocean, Surface Winds, Tasmania, fugacity, pCO2, partial pressure
Organization: CSIRO Oceans & Atmosphere - Hobart