Davidson Current
In oceanography, the Davidson Current is a coastal :wikt:countercurrent|countercurrent of the Pacific Ocean running north along the western coast of the United States from Baja California, Mexico to northern Oregon, ending at about latitude 48°N.
Its flow is adjacent to the California Current, but it flows north rather than south and hugs the coastline. The current is active year-round at 650 feet below sea level, but surfaces during the winter months, generally from mid-November through mid-February. In these months, northerly winds weaken and are replaced to some extent by southwesterly winds.
The Davidson Current was discovered by the American geodesist, astronomer, geographer, surveyor and engineer George Davidson.
