A simple plankton model for the Oregon upwelling ecosystem: Sensitivity and validation against time-series ocean data

• Published in: Ecological modelling 2011-03, Vol.222 (6), p.1222-1235
• Main Authors: Ruzicka, James J., Wainwright, Thomas C., Peterson, William T.
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Biomass; chlorophyll; Dynamical systems; Dynamics; Ecosystems; Fundamental and applied biological sciences. Psychology; General aspects; General aspects. Techniques; Marine; Mathematical models; Methods and techniques (sampling, tagging, trapping, modelling...); model validation; Northern California Current; nutrient uptake; Nutrients; Oregon; Parameter; Phytoplankton; Plankton; Plankton model; Retention mechanism; Sensitivity; Synecology; Upwelling
• ISSN: 0304-3800; 1872-7026
• DOI: 10.1016/j.ecolmodel.2011.01.001

► A plankton model was developed for the Northern California Current upwelling ecosystem. ► Model estimates of nutrient concentration, phytoplankton biomass, and zooplankton biomass were compared to time-series observations made across the central Oregon shelf. Such an extensive model to data comparison is unique among the models developed for the California Current system. ► A sensitivity analysis is run to identify the parameters to which the model is most sensitive and to see how alternate parameterization strategies effect model quality when compared to observations. ► The role of potential zooplankton behavioral retention mechanisms is tested in terms of its effect on biomass, cross-shelf distribution, and model quality compared to observation. Simple plankton models serve as useful platforms for testing our understanding of the mechanisms underlying ecosystem dynamics. A simple, one-dimensional plankton model was developed to describe the dynamics of nitrate, ammonium, two phytoplankton size-classes, meso-zooplankton, and detritus in the Oregon upwelling ecosystem. Computational simplicity was maintained by linking the biological model to a one-dimensional, cross-shelf physical model driven by the daily coastal upwelling index. The model sacrificed resolution of regional-scale and along-shore (north to south) processes and assumed that seasonal productivity is primarily driven by local cross-shelf Ekman transport of surface waters and upwelling of nutrient-rich water from depth. Our goals were to see how well a simple plankton model could capture the general temporal and spatial dynamics of the system, test system sensitivity to alternate parameter set values, and observe system response to the effective scale of potential retention mechanisms. Model performance across the central Oregon shelf was evaluated against two years (2000–2001) of chlorophyll and copepod time-series observations. While the modeled meso-zooplankton biomass was close in scale to the observed copepod biomass, phytoplankton was overestimated relative to that inferred from the observed surface chlorophyll concentration. Inshore, the system was most sensitive to the nutrient uptake kinetics of diatom-size phytoplankton and to the functional grazing response of meso-zooplankton. Meso-zooplankton was more sensitive to alternate parameter values than was phytoplankton. Reduction of meso-zooplankton cross-shelf advection rates (crudely representing behavioral retention mechanisms) red