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Measurements taken onboard R/V Kaimimoana between 1999 and 2002
Measurements from the NOAA ship, the Kaimimoana between 1999 and 2002.
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Measurements made by the NOAA R/V Ron H. Brown
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Measurements made by the NOAA research vessel, the Ron H. Brown between 2000 and 2002.
Measurements made onboard the R/V MIRAI between 2000 and 2003
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Measurements made by the MIRAI research vessel in the JAMSTEC fleet between 2000 and 2003.
Measurements made by the Akademik Kurchatov Russian research vessel
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Measurements made by the Akademik Kurchatov Russian research vessel in the Atlantic Ocean and Black Sea in 1988.
Measurements made by the Akademik Ioffe Russian vessel
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Measurements made by the Akademik Ioffe Russian vessel along a Atlantic Meridional Transect in 2001 to 2002.
Measurements from the Sea of Japan between 1999 and 2000
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Measurements from the Sea of Japan made between 1999 and 2000.
Measurements from the western equatorial Pacific Ocean
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Measurements taken in the western equatorial Pacific Ocean in 1996.
Partial pressure (or fugacity) of carbon dioxide, water temperature, salinity and other variables collected from surface underway observations during NOAA Ship Oceanographer, NOAA Ship Discoverer, and R/V Akademik Korolyov cruises in the Pacific and Indian Oceans from 1986-05-21 to 1989-04-20 (NCEI Accession 0000071)
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This dataset includes Partial pressure (or fugacity) of carbon dioxide, water temperature, salinity and other variables collected from surface underway observations during NOAA Ship Oceanographer, NOAA Ship Discoverer, and R/V Akademik Korolyov cruises in the Pacific and Indian Oceans from 1986-05-21 to 1989-04-20. These cruises were conducted under support from the National Oceanic and Atmospheric Administration (NOAA). Carbon dioxide measurements in the atmosphere and in surface water were made by analyzing of mixing ratios of CO2 with an automated, temperature-controlled gas chromatographic system described by Murphy et al. (1991) and Bates et al. (1993). Instrument precision was determined by the average percent standard deviation of the standard response over a 6-hour period. The precision varied between cruises but was always less than 1.2% and was more typically around 0.4%. Air was pumped through 3/8-inch diameter, plastic-coated, aluminum tubing from the jackstaff on the bow of the ship (10 meters above the sea surface) to the oceanographic laboratory for analysis. Surface seawater entered the ship via a forward intake line located approximately 5 meters below the water level.
Turbidity, SOLAR RADIATION - ATMOSPHERIC and other data from NOAA Ship SURVEYOR in the North Pacific Ocean, Bering Sea and NE Pacific from 1995-09-10 to 1995-09-19 (NCEI Accession 9600139)
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Hydrophysical, hydrochemical, and other data were collected from NOAA Ship SURVEYOR from September 10, 1995 to September 19, 1995. Data were submitted by Mr. David Kachel from the US DOC; NOAA; ENVIRONMENTAL RESEARCH LABORATORY; PACIFIC MARINE ENVIRONMENTAL LABORATORY. These data were collected using meteorological sensors, Secchi disks, transmissometers, bottle casts, and CTD casts in the Northeast Pacific Ocean.
Measurements made in the west-central Pacific near Wake Island
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Measurements made in the west-central Pacific near Wake Island in 2007.
WATER TEMPERATURE and other data from NOAA Ship DISCOVERER from 1982-05-12 to 1986-10-31 (NCEI Accession 9900053)
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