This dataset includes surface chemical, physical and time series data collected from Mooring_Östergarnsholm_57.4N_19E in the Baltic Sea from 2005-05-31 to 2022-10-20. These data include Partial pressure (or fugacity) of carbon dioxide - water and sea surface temperature. The instruments used to collect these data include bubble type equilibrator for autonomous carbon dioxide (CO2) measurement and Carbon dioxide (CO2) gas analyzer. The Global CO2 Time-series and Moorings Project involves international groups from 18 countries who have mounted sensors on moored buoys to provide high resolution time-series measurements of atmospheric boundary layer and surface ocean CO2 partial pressure (pCO2). The CO2 Time-series and Moorings Project is coordinated by UNESCO International Ocean Carbon Coordination Project (IOCCP).

This dataset includes surface underway chemical, meteorological and physical data collected during R/V Arni Fridriksson cruises in the Irminger Sea and North Atlantic Ocean from 2024-05-04 to 2024-05-21. These data include measurements of sea surface temperature (SST), equilibrator temperature (TEQ), equilibrator pressure (PEQ), mole fraction of carbon dioxide (xCO2) in dry air at TEQ, pCO2 at TEQ (PCO2TEQ). The instruments used to collect these data include carbon dioxide (CO2) gas analyzer and shower head chamber equilibrator for autonomous CO2 measurement.

This dataset includes surface underway measurements of partial pressure of carbon dioxide (pCO2) in water and atmosphere, sea surface temperature, sea surface salinity and barometric pressure collected during the M/V Tavastland cruises in the Baltic Sea in from 2020-01-07 to 2020-06-15. A General Oceanics (GO) pCO2 system (model 8050) was used for pCO2 measurements. The system is described in detail in Pierrot (2009). Surface water is pumped continuously from the intake to the equilibrator. The equilibrator contains a water spray head, and as the water flows through it the dissolved CO2 equilibrates with the headspace. The headspace is dried and xCO2 is determined by an infrared sensor. Calculations were performed following Pierrot (2009). The water is drawn directly from the sea chest at 6m depth. A temperature sensor (SBE38) is installed close to the intake. The water is pumped through 5 m of a piping connecting to the GO system. The equilibrator pressure is measured using a differential pressure sensor (inside/outside equilibrator) and an absolute pressure sensor next to the equilibrator. The air inlet is located 30 m above sea level next to the ship's funnel and the air line is constantly flushed with atmospheric air.

This dataset includes surface underway chemical, meteorological and physical data collected during R/V Arni Fridriksson cruises in the Irminger Sea and North Atlantic from 2006-11-07 to 2015-10-04. These data include measurements of sea surface temperature (SST), equilibrator temperature (TEQ), equilibrator pressure (PEQ), mole fraction of carbon dioxide (xCO2) in dry air at TEQ, pCO2 at TEQ (PCO2TEQ). The instruments used to collect these data include carbon dioxide (CO2) gas analyzer and shower head chamber equilibrator for autonomous CO2 measurement.

This dataset includes Surface underway, chemical and meteorological data collected from POLARSTERN in the Adriatic Sea, Aegean Sea, Alboran Sea, Arabian Sea, Balearic (or Iberian) Sea, Baltic Sea, Bay of Bengal, Bay of Biscay, Bay of Fundy, Black Sea, Bristol Channel, Caribbean Sea, English Channel, Gulf of Aden, Gulf of Aqaba, Gulf of Guinea, Gulf of Oman, Gulf of Riga, Gulf of St. Lawrence, Gulf of Suez, Hudson Strait, Indian Ocean, Inner Sea - West Coast Scotland, Ionian Sea, Irish Sea and St. George's Channel, Kattegat, The Sound, Great Belt, Little Belt, Labrador Sea, Laccadive Sea, Ligurian Sea, Mediterranean Sea, Mediterranean Sea - Eastern Basin, Mediterranean Sea - Western Basin, North Atlantic Ocean, North Sea, Persian Gulf (Gulf of Iran), Red Sea, Sea of Azov, Sea of Marmara, Skagerrak, South Atlantic Ocean, Strait of Gibraltar and Tyrrhenian Sea from 2014-03-09 to 2015-01-31. These data include BAROMETRIC PRESSURE, Partial pressure (or fugacity) of carbon dioxide - atmosphere, Partial pressure (or fugacity) of carbon dioxide - water, WIND DIRECTION and WIND SPEED. The instruments used to collect these data include Carbon dioxide (CO2) gas analyzer. These data were collected by Mario Hoppema of Alfred Wegener Institute for Polar and Marine Research (AWI) and Steven M. A. C. van Heuven of Groningen University as part of the VOS_Polarstern_06AQ20140309, VOS_Polarstern_06AQ20140608, VOS_Polarstern_06AQ20140707, VOS_Polarstern_06AQ20140805, VOS_Polarstern_06AQ20141026 and VOS_Polarstern_06AQ20141203 dataset. CDIAC associated the following cruise ID(s) with this dataset: 06AQ20140309, 06AQ20140608, 06AQ20140707, 06AQ20140805, 06AQ20141026 and 06AQ20141203

This dataset includes partial pressure (or fugacity) of carbon dioxide, dissolved inorganic carbon, temperature, salinity, nutrients and dissolved oxygen collected from discrete samples and profile observations during the R/Vs Arni Fridriksson and Bjarni Saemundsson time series IcelandSea (LN6) cruises in the North Atlantic Ocean from 1985-02-22 to 2013-11-26.

This dataset includes surface underway measurements of partial pressure of carbon dioxide (pCO2) in water and atmosphere, sea surface temperature, sea surface salinity and barometric pressure collected during the M/V Tavastland cruises in the Baltic Sea in from 2021-05-01 to 2021-12-06. A General Oceanics (GO) pCO2 system (model 8050) was used for pCO2 measurements. The system is described in detail in Pierrot (2009). Surface water is pumped continuously from the intake to the equilibrator. The equilibrator contains a water spray head, and as the water flows through it the dissolved CO2 equilibrates with the headspace. The headspace is dried and xCO2 is determined by an infrared sensor. Calculations were performed following Pierrot (2009). The water is drawn directly from the sea chest at 6m depth. A temperature sensor (SBE38) is installed close to the intake. The water is pumped through 5 m of a piping connecting to the GO system. The equilibrator pressure is measured using a differential pressure sensor (inside/outside equilibrator) and an absolute pressure sensor next to the equilibrator. The air inlet is located 30 m above sea level next to the ship's funnel and the air line is constantly flushed with atmospheric air.

This dataset includes surface underway chemical, meteorological and physical data collected from R/V Bjarni Saemundsson cruises in the Irminger Sea, Iceland Sea and North Atlantic from 2006-05-14 to 2019-10-21. These data include measurements of sea surface temperature (SST), equilibrator temperature (TEQ), equilibrator pressure (PEQ), mole fraction of carbon dioxide (xCO2) in dry air at TEQ, pCO2 at TEQ (PCO2TEQ). The instruments used to collect these data include carbon dioxide (CO2) gas analyzer and shower head chamber equilibrator for autonomous CO2 measurement.

This dataset includes surface underway measurements of partial pressure of carbon dioxide (pCO2) in water and atmosphere, sea surface temperature, sea surface salinity and barometric pressure collected during the M/V Tavastland cruises in the Baltic Sea in from 2019-10-02 to 2020-01-02. A General Oceanics (GO) pCO2 system (model 8050) was used for pCO2 measurements. The system is described in detail in Pierrot (2009). Surface water is pumped continuously from the intake to the equilibrator. The equilibrator contains a water spray head, and as the water flows through it the dissolved CO2 equilibrates with the headspace. The headspace is dried and xCO2 is determined by an infrared sensor. Calculations were performed following Pierrot (2009). The water is drawn directly from the sea chest at 6m depth. A temperature sensor (SBE38) is installed close to the intake. The water is pumped through 5 m of a piping connecting to the GO system. The equilibrator pressure is measured using a differential pressure sensor (inside/outside equilibrator) and an absolute pressure sensor next to the equilibrator. The air inlet is located 30 m above sea level next to the ship's funnel and the air line is constantly flushed with atmospheric air.