California Current, surface oceanic current, southward-flowing continuation of theAleutian Current along the westcoast ofNorth America between latitudes 48° N and 23° N. The California Current’s surface velocity is commonly less than 10 inches. (25 cm) per second, transporting about 390,000,000 cubic feet (11,000,000 cubic metres) of water per second above 3,300 feet (1,000 metre).

The temperature and salinity of its waters vary with seasonal variations in upwelling, insolation, and flow. The maximum ranges in temperature and salinity from its northern to its southern end are 48 to 79 °F (9 to 26 °C) and 32.5 to 34.5 parts per thousand, respectively. During the summer, when upwelling is most dominant, a countercurrent below 650 feet develops close to the coast. The cold upwelling water brings rich nutrients to the surface andabundant plankton and animal life is supported.