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The model simulations also show skill representing increases in groundwater storage (1981 1982 and 1995 1998), but these simulated increases are of lower magnitude than the observed changes.
The model simulations also allow investigations into the causes and predictability of extreme events, but this is beyond the scope of this study.
Moreover, the model simulations also suggest that additional contaminant spillages have occurred in 2012.
Model simulations also showed that it is possible to predict nuclei size distributions beyond the drop controlled nucleation regime in Hapgood's nucleation regime map.
The model simulations also provided the base to analyse the cumulative effects caused by the habitat degradation that can ultimately lead to the extinction of local populations.
Climate model simulations also support the view that the EASM was already active during the Eocene, probably because of higher atmospheric pCO2 at that time (Huber and Goldner 2012; Zhang et al. 2012a; Licht et al. 2014).
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Model simulation also found out that the optimal phosphate concentration was approximately 10.3 mM for 100 mM sucrose, which was validated by experimental data.
Policy rule prescriptions, particularly prescriptions that are obtained from a dynamic model simulation, also help policymakers take to heart a key message of the literature on policy rules namely, that monetary policy decisions should concern the appropriate path for the policy instrument and not merely the current setting of that instrument.
Wang et al. (2014) in a coupled WAM/ionosphere model simulation also found a phase shift of the SW2 solar component during SSWs caused by SSW-induced variability in its main source, stratospheric ozone, and/or additional middle atmosphere circulation changes.
The model simulation also shows that the delay can enhance the amplitude of the periodic solution when the periodic solutions exist, which means that the delay has a large effect on the dynamics of system (4), as proved in Figure 7.
However, our model simulation also predicts an aerosol enhancement mainly composed of mineral dust extending from the surface up to 13 km above Africa, Box 2, which is not seen in the CALIPSO [ Vernier et al., 2011a] or SAGE II [ Thomason and Vernier, 2013] observations.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com