AndreaBozzo/ceres-open-data-index huggingface dataset:
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS022009 Leg 2

This data was collected in May and June 2009 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS022009 Leg 2.

Departed:  Nuku'Alofa, Tonga, May 28, 2009
Arrived: 	Lautoka Fiji, June 25, 2009


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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Bluewater and Climate, Carbon Dioxide Measurements, Countries, Fiji, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Pacific Ocean, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tonga, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS022009 Leg 1

This data was collected in April and May 2009 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS022009 Leg 1.

Departed: 	Lautoka Fiji, April 22, 2009
Arrived:  	Nuku'Alofa, Tonga, May 18, 2009

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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Bluewater and Climate, Carbon Dioxide Measurements, Countries, Fiji, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Pacific Ocean, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tonga, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP-XBT Upper Ocean Thermal Data collected on the line PX35 (Melbourne - Dunedin)

This dataset contains temperature data obtained from XBTs (expendable bathythermographs) deployed by vessels during different cruises between Melbourne (Australia) and Dunedin (New Zealand).

Expendable Bathythermographs (XBTs) have been used for many years by oceanographers to measure the temperature of the upper ocean. These instruments are simple devices which are designed to be deployed from moving vessels, enabling broad scale coverage of the world's oceans.

Tags: Australia, Bathythermographs, Bluewater and Climate, Countries, Expendable Bathythermographs, IMOS Node, IMOS Sub-Facility, New Zealand, Ocean Pressure, Ocean Temperature, Oceans, Pacific Ocean, SOOP-XBT, Water Pressure, Water Temperature
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP Sea Surface Temperature data collected on the Merchant Vessel Wana Bhum

This dataset contains Sea Surface Temperature (SST) underway observations collected on trips of a merchant vessel Wana Bhum (callsign HSB3403). This data stream has now been discontinued (April 2013). 

Bulk SST is measured by SBE48 hull contact sensor. The sensor is installed in the bow thruster room at 8.5m depth. 

Observed data are 1-minute median SST values and are retrieved from the vessel once an hour and quality controlled at the Bureau of Meteorology. A daily file is available after 0100 UTC. High-resolution 1-minute median data are available in the delayed mode approximately every 3 months.

Tags: Ocean Temperature, Oceans, Sea Surface Temperature
Organization: Bureau of Meteorology (BOM)
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS022008

This data was collected in February 2008 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS022008.

Departed: 	Hobart, Tasmania, February 04, 2008
Arrived:  	  Port Adelaide, South Australia, February 26, 2008

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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, South Australia, Southern Ocean, Surface Winds, Tasmania, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP Underway Data from AIMS Vessel RV Solander Trip 6682 From 16 Mar 2017 To 23 Mar 2017

'Ships of Opportunity' (SOOP) is a facility of the Australian 'Integrated Marine Observing System' (IMOS) project. This data set was collected by the SOOP sub-facility 'Sensors on Tropical Research Vessels' aboard the RV Solander Trip 6682.

Instrumentation was deployed for measuring Seawater Intake Temperature at 1.9m  on trip 6682 from 16 Mar 2017 through to 23 Mar 2017, and the installation was located at/on RV Solander. Sensor deployed was a SBE 38 remote temperature sensor manufactured by Sea-Bird Electronics, Inc., model SBE 38. 

Instrumentation was deployed for measuring Salinity at 1.9m  on trip 6682 from 16 Mar 2017 through to 23 Mar 2017, and the installation was located at/on RV Solander. Sensor deployed was a SBE 21 conductivity cell manufactured by Sea-Bird Electronics, Inc., model SBE 21. 

Instrumentation was deployed for measuring Turbidity at 1.9m  on trip 6682 from 16 Mar 2017 through to 23 Mar 2017, and the installation was located at/on RV Solander. Sensor deployed was a Wet Labs FLNTU-RT Optical sensor (Turbidity and Fluorescence) manufactured by Wetlabs, model FLNTU-RT. 

Instrumentation was deployed for measuring Fluorescence at 1.9m  on trip 6682 from 16 Mar 2017 through to 23 Mar 2017, and the installation was located at/on RV Solander. Sensor deployed was a Wet Labs FLNTU-RT Optical sensor (Turbidity and Fluorescence) manufactured by Wetlabs, model FLNTU-RT.

Tags: Bathymetry, Biological Oceanography, Chemical Oceanography, Conductivity, EARTH SCIENCES, Fluorescence, IMOS Sub-Facility, Ocean Chemistry, Ocean Optics, Ocean Temperature, Oceanography, Oceans, Physical Oceanography, SOOP-TRV, Sensors on Tropical Research Vessels, Thermosalinographs, Turbidity, Water Temperature
Organization: Australian Institute of Marine Science
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS012010 (Sydney-Hobart)

This data was collected in January and February 2010 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS012010.

Departed:  Sydney, Australia, January 22, 2010
Arrived:  	 Hobart, Australia, February 15, 2010

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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, Countries, Fugacity, IMOS Node, IMOS Sub-Facility, New South Wales, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Pacific Ocean, Partial Pressure, Regional Seas, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tasman Sea, Tasmania, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS012009

This data was collected in February and March 2009 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS012009.

Departed: 	Wellington, New Zealand, February 03, 2009
Arrived:  	Nuku'Alofa, Tonga, February 25, 2009
Departed: 	Nuku'Alofa, Tonga, February 26, 2009
Arrived:  	Lautoka, Fiji, March 23, 2009

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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Bluewater and Climate, Carbon Dioxide Measurements, Countries, Fiji, Fugacity, IMOS Node, IMOS Sub-Facility, New Zealand, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Pacific Ocean, Partial Pressure, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tonga, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS012008

This data was collected in January 2008 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS012008.

Departed: 	Hobart, Tasmania, January 11, 2008
Arrived:  	Hobart, Tasmania February 01, 2008

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 four hours to calibrate the gas analyser. The standard gas concentrations are on the WMO-X2007 mole fraction scale for CO2-in-air. 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 located at about 5.5m depth in the bow of the ship. Sea surface salinity is measured using a thermosalinograph (Seabird Electronics SBE21) located next to the CO2 system. A remote temperature sensor (Seabird Electronics SBE 38) located at the intake is used to measure sea surface temperature (SST). The travel time between the intake and CO2 system is typically about 4 minutes with warming usually less than 0.6ºC. The thermosalinograph water is from the same intake, but the supply lines separate after the intake. A comparison of thermosalinograph and equilibrator temperature records shows the temperature difference in the two lines is generally less than 0.1ºC. The thermosalinograph water line travels outside the ship and is typically warmer than the equilibrator. The travel time in water line to the thermosalinograph is 2.5 minutes faster than to the equilibrator. 

Meteorological data, salinity, SST, and ships position and time are taken from the ships logging system. These parameters and the data quality are maintained by the Australian Marine National Facility.

Tags: Atmosphere, Atmospheric Pressure, Australia, Bluewater and Climate, Carbon Dioxide Measurements, 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, Tasmania, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP-XBT Upper Ocean Thermal Data collected on the line PX33 (Hobart - Macquarie Island)

Temperature data from the TOGA/WOCE transect PX33 between Hobart and Macquarie Island has been collected since december 1992 and are ongoing. The transect is repeated irregularly.
The data are obtained from XBTs (expendable bathythermographs) deployed by the French Antarctic resupply vessel L'Astrolabe, and are managed by the  French Polar Institute (IPEV) and 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: Bathythermographs, Bluewater and Climate, Expendable Bathythermographs, IMOS Node, IMOS Sub-Facility, Macquarie Island, Ocean Pressure, Ocean Temperature, Oceans, SOOP-XBT, Southern Ocean, Water Pressure, Water Temperature
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Aurora Australis voyage AA2011VMS (Hobart-Hobart)

This data was collected in January/February 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Aurora Australis (IMOS platform code: VNAA) voyage AA1011_VMS.

Departed: 	Hobart, Tasmania, 	    	January 04, 2011
Arrived:  	Hobart, Tasmania, 		February 07, 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