Chlorophyll-A Front Strength describes the gradient magnitude of fronts derived from chlorophyll-a concentration at the ocean surface for Spring, Summer, Fall, and Winter, in units of log(mg / m3) / km.
Oceanic fronts are areas of sharp gradients between adjacent water masses that occur across large spatial and temporal scales. In the California Current System (CCS), fronts are created by wind-driven upwelling and the flow of the upwelled water in the form of cold, chlorophyll-rich filaments and eddies. Fronts are indicators of many oceanographic processes and are sites of increased biological activity affecting all oceanic life forms from microbes to seabirds and marine mammals.
These data were derived from the NOAA CoastWatch (dataset: erdMEchla1day; 2002-2013).