What have we done about it?
Increased sophistication of satellite algorithms
Addition of phytoplankton functional groups
Addition of elements
Increased realism of physical models
Spatial resolution (mesoscale eddies)
Temporal variability (El Nino; NAO; PDO)
Better physics (Gent-McWilliams; KPP)
Distinguishing regions of nitrogen, phosphorus,
silicon and iron limitation