Chemical, physical, and other data were collected from NOAA Ship DAVID STARR JORDAN from June 08, 1975 to June 11, 1975. Data were collected using meteorological sensors, Secchi disk, and bottle casts. Data were submitted by Scripps Institution of Oceanography (SIO) as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Chemical, physical, and other data were collected from the NEW HORIZON from November 12, 1980 to November 12, 1980. Data were collected using meteorological sensors, Secchi disk, and bottle casts. Data were submitted by Scripps Institution of Oceanography (SIO) as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Chemical, physical, and other data were collected from NOAA Ship DAVID STARR JORDAN and NEW HORIZON from January 28, 1992 to October 14, 1994. Data were collected using fluorometer, laboratory analysis, visual analysis, and bottle casts in the Northeast Pacific Ocean. Data were submitted by Scripps Institution of Oceanography (SIO) as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Chemical, physical, and other data were collected from the A. AGASSIZ from November 10, 1966 to November 13, 1966. Data were collected using meteorological sensors, Secchi disk, and bottle casts. Data were submitted by Scripps Institution of Oceanography (SIO) as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Chemical, physical, and other data were collected from NOAA Ship DAVID STARR JORDAN, ROGER REVELLE, and NEW HORIZON from August 7, 1996 to April 19, 1997. Data were collected using bottle casts in the Pacific Ocean. Data were submitted by Scripps Institution of Oceanography (SIO) as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Temperature, pressure, conductivity, salinity, bottom depth, and other data were collected using meteorological sensors, and thermosalinograph from NOAA Ship DAVID STARR JORDAN from January 24, 2002 to December 08, 2002. Data were collected in the Coastal waters of western US and the Northeast Pacific Ocean. Data were submitted by the US DOC; NOAA; OFFICE OF NOAA CORPS OPERATIONS as a part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Temperature, pressure, conductivity, salinity, bottom depth, and other data were collected using meteorological sensors, and thermosalinograph from NOAA Ship DAVID STARR JORDAN from January 5, 2004 to July 7, 2004. Data were collected in the Coastal Waters of Western US and the Northeast Pacific Ocean. Data were submitted by the Office of NOAA Corps Operations as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Temperature, pressure, conductivity, salinity, bottom depth, and other data were collected using meteorological sensors, and thermosalinograph from NOAA Ship DAVID STARR JORDAN from July 12, 2004 to August 8, 2004. Data were collected in the Coastal Waters of Western US and the Northeast Pacific Ocean. Data were submitted by the Office of NOAA Corps Operations as part of the California Cooperative Fisheries Investigation (CALCOFI) project.

Chemical, physical, and other data were collected using bottle, BT, current meter, MBT, meteorological sensors, and Secchi disk casts from January 1, 1968 to December 4, 1968. Data were submitted by Stanford University; Hopkins Marine Station as part of the California Cooperative Fisheries Investigation (CALCOFI) project. Data were processed by NODC to the NODC standard F004 water physics and chemistry format. The F004 format contains data from measurements and analysis of physical and chemical characteristics of the water column. Chemical parameters that may be recorded are salinity, pH and concentration of oxygen, ammonia, nitrate, phosphate, chlorophyll and suspended solids. Physical parameters that may be recorded include temperature, density (sigma-t), transmissivity and current velocity (east-west and north-south components). Cruise and station information may include environmental conditions of the study site at the time of observation. Data are very sparse prior to 1951.

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