Comparisons between simulations using the model and measurements from a real container show an average error of less than ±1K on the states important for control.
Although no substantial difference is observed between simulations using the simpler two-compartment cytosol model or the multishell eight-compartment cytosol model and no advantage is gained from using the larger and slower model, it is adopted here to give comparability with Zeuthen's et al. (7, 9, 22) and Lapointe's (3, 5) models for simulation across GLUT2.
The sea surface temperature differences between the simulations using the uncoupled and coupled models are shown in Figure 11.
In Table 1, we compare the average execution times, average total distances, and average speeds of robots between the simulations using the Space D* and the simulations using only the D*.
Therefore, we compared the horizontal simulated sea surface temperature distributions (Figure 10f,g,h,i,j) and the differences between the simulations using the uncoupled and coupled models (Figure 11) with those for the TRMM/TMI sea surface temperatures (Figure 3e,f,g,h), and the differences between before and after the typhoon had passed (Figure 3i,j,k,l).
A comparison between TFM simulations using the present KTGF model, and a more simple kinetic theory for rapid flow of slightly frictional, nearly elastic spheres derived by Jenkins and Zhang (2002), is carried out to investigate the influence of particle friction in the fluidized bed.
In fact, fairly little changed between the simulations using the standard FBA formulation and those accounting for molecular crowding.
We perform a direct quantitative comparison, across a range of operating conditions, between laboratory scale experiments and simulations using the discrete element method (DEM).
The fitted parameters are estimated by minimizing the squared error between log10 transformed data and simulations, using the pattern search optimizer in the MATLAB Global Optimization Toolbox.
Comparisons between uniaxial monotonic data and FE simulations using the model show a very good agreement.
To further check the relative energetics of the three terminations and resulting surfaces we added 53 H2O molecules between the slabs and ran AIMD simulations using the PBE96 exchange correlation functional for at least 10 ps.
