five

LIFECO: Coupled Bio-Physical Modelling: Simulation of lower trophic level dynamics

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This work package is part of the LIFECO programme: LInking Hydrographic Frontal activity to ECOsystem dynamics in the North Sea and Skagerrak: Importance to fish stock recruitment. The key to resolving the influence of frontal processes on the distribution and production of planktonic organisms, the so-called bottom up processes influencing ecosystem dynamics, is quantifying the effects of frontal manifestations on intra and interannual variations in: population growth and production rates due to fluxes of nutrients limiting primary production and; rates of aggregation of organisms due to the interaction between behavioural patterns (e.g. diel migration) and frontal circulation patterns. Once these two mechanisms have approximated realistically the effects of variations of frontal activity (due to climatic forcing) on the bottom up processes can be quantified. In order to accomplish these goals, this work package will couple NORWegian ECOlogical Model (NORWECOM; a nutrient based 3-D primary production model previously developed by partner 7 inside the HAMSOM(WP1) for the estimation of increases in primary and secondary production due to frontal mixing processes extend the nested HAMSOM from WP1: Advancement of Hydrodynamic models, a particle-tracking model for passive tracers to include the active migration of planktonic organisms observed during the field component of the program performed in WP 4: Distribution and Abundance of plankton and fish relative frontal processes. Nutrient based primary production models using intermediate grid scales have been developed for the North Sea ecosystem as well as for other systems. These models have been used to estimate rates of primary and secondary production as well as to examine the effect of variations in climatic forcing on primary production. However, again the resolution in these earlier exercises is insufficient for the investigation of processes in and around fronts. Therefore, the 1-km nested model developed in WP1 will provide the platform for running a particle-tracking model on the same grid scale. The coupling of these two approaches will provide simulated horizontal and vertical distributions of planktonic biomass due to nutrient fluxes/enhanced production and aggregation of organisms in and around the frontal regimes for comparison with field observations (WP4 & 5) in 2001. Furthermore, this approach will allow the simulation of intra and inter-annual variations in the spatial and temporal distributions of primary and secondary production for the years 2000 to 2002 as well as years exhibiting anomalous recruitment success in key fish stocks or climatic conditions. Hence generating hypotheses and data bases to be utilised in work package 9: Synthesis, scenario and hypothesis testing.
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