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[Top](Hydrodynamics)
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# Calibration exchange rates
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To calculate the exchange rates between the compartments and the North Sea, tracer simulations have also been run for the different schematizations (0D, 4Comp and 28Comp) of the DEMO model. The exchange rates between the compartments are calculated by fitting the model output of the DEMO model to the data generated by the GetM/GotM model.
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To calculate the exchange rates between the compartments and the North Sea, tracer simulations have also been run for the different schematizations (0D, 4Comp and 28Comp) of the DEMO model. The exchange rates between the compartments are calculated by fitting the model output of the DEMO model to the data generated by the GetM/GotM model. For each hour, the average tracer concentration within each compartment has been calculated. The models are fitted by changing the exchange rates between the compartments using the modFit function in R (Soetaert and Petzold, 2010)[^3228].
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# References
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[^3049]: Jiang, L., T. Gerkema, J. W. M. Wijsman en K. Soetaert (2019) Comparing physical and biological impacts on seston renewal in a tidal bay with extensive shellfish culture. Journal of Marine Systems 194: [link](https://doi.org/10.1016/j.jmarsys.2019.03.003)
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[^3228]: Soetaert, K. and T. Petzoldt (2010) Inverse Modelling, Sensitivity and Monte Carlo Analysis in R Using Package FME. Journal of Statistical Software 33(3): 1:28.[link](http://www.jstatsoft.org/v33/i03/) |
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