AndreaBozzo/ceres-open-data-index huggingface dataset:
IMOS SOOP Underway Data from AIMS Vessel RV Solander Trip 6807 From 22 Sep 2017 To 24 Sep 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 6807.

Instrumentation was deployed for measuring Seawater Intake Temperature at 1.9m  on trip 6807 from 22 Sep 2017 through to 24 Sep 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 6807 from 22 Sep 2017 through to 24 Sep 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 6807 from 22 Sep 2017 through to 24 Sep 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 6807 from 22 Sep 2017 through to 24 Sep 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 SS2011_V01 (Hobart-Hobart)

This data was collected in April 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_V01.

Departed: 	Hobart, TAS, Apr 16, 2011
Arrived:   	Hobart, TAS, Apr 21, 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 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, Hobart, IMOS Node, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, Salinity, Sea Surface Temperature, Southern Ocean, States, Surface Winds, TAS, Tasmania, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS SOOP Sea Surface Temperature data collected on the Merchant Vessel Xutra Bhum

This dataset contains Sea Surface Temperature (SST) underway observations collected on trips of a merchant vessel Xutra Bhum (callsign HSB3402). 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 SS2011_T04 (Fremantle-Hobart)

This data was collected in November 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_T04.

Departed: 	Fremantle, WA,   Nov 10, 2011
Arrived:   	Hobart, TAS,   Nov 20, 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 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, Indian Ocean, 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 RV Southern Surveyor voyage SS2011_T03 (Hobart-Fremantle)

This data was collected in August 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_T03.

Departed: 	Hobart, TAS,   Aug 12, 2011
Arrived:   	Fremantle, WA,   Aug 22, 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 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, Indian Ocean, 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 RV Southern Surveyor voyage SS2011_T02 (Auckland-Hobart)

This data was collected in June 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_T02.

Departed: 	Auckland, NZ,   June 06, 2011
Arrived:   	Hobart, TAS,   June 14, 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 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 Zealand, Ocean Biogeochemistry, Ocean Temperature, Ocean Winds, Oceans, Partial Pressure, Regional Seas, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tasman Sea, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS2011_T01 (Hobart-Brisbane)

This data was collected in May 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_T01.

Departed: 	Hobart, 	   TAS, May 04, 2011
Arrived:   	Brisbane, QLD, May 12, 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 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, Queensland, Regional Seas, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, Tasman Sea, Tasmania, Victoria, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart
IMOS - SOOP Ocean Carbon Dioxide Data from RV Southern Surveyor voyage SS2011_C01 (Sydney-Hobart)

This data was collected in April 2011 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2011_C01.

Departed: 	Sydney, NSW, Apr 05, 2011
Arrived:   	   Hobart, TAS, Apr 14, 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 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 SS2010_V09 (Sydney-Sydney)

This data was collected in October 2010 by the IMOS Ship of Opportunity Underway CO2 Measurement research group on RV Southern Surveyor (IMOS platform code: VLHJ) voyage SS2010_V09.

Departed: 	Sydney, NSW, Oct 14, 2010
Arrived:  	Sydney, NSW, Oct 31, 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, SOOP-CO2, Salinity, Sea Surface Temperature, Surface Winds, pCO2
Organization: CSIRO Oceans & Atmosphere - Hobart