Spatial and temporal variabilities of the chlorophyll distribution in the northeastern tropical Pacific: The impact of physical processes on seasonal and interannual time scales

A global eddy-resolving coupled physical–biological model is used to investigate the seasonal and interannual variabilities of the chlorophyll in the northeastern tropical Pacific during 2000–2007. The seasonal variability of the surface chlorophyll concentration in the model agrees well with satellite ocean color data, except for the equatorial region. High chlorophyll levels off the Gulf of Tehuantepec, Papagayo, and Panama in winter and in the Costa Rica Dome in summer are well reproduced. Production in these areas is controlled by the supply of nitrate rich-waters through vertical mixing and coastal and open ocean upwelling. The variability of the thermocline depth is strongly connected to the seasonal variability of surface chlorophyll. El Niño Southern Ocean (ENSO) variability has a marked effect on the marine ecosystem. The model reproduces the variability of chlorophyll corresponding to the observed ENSO variability. During cold SST anomaly phases (2000, 2001 and 2007), the chlorophyll concentration is considerably higher than other years (2002–2006). Chlorophyll variance is largest off the Gulf of Papagayo and over the Costa Rica Dome where the changes to chlorophyll levels are related to changes in the supply of nitrate rich-waters through vertical mixing and upwelling.

► We investigated the chlorophyll variability in the eastern tropical Pacific by model. ► High chlorophylls off the three gulfs and in the Costa Rica Dome are reproduced. ► The thermocline depth is strongly connected to the seasonal chlorophyll variability. ► The model reproduces the chlorophyll variability corresponding to the observed ENSO. ► During cold SST anomaly phases, the chlorophyll concentration is considerably high.