The similar pattern of bias found for simulations with simulated and observed pedigrees suggests that this bias may be caused much more by the nature of the two-step approach than by data structure.
Two averaged simulated cell density profiles for simulations with D = 81 μmhour−1 at t=48 hours using low cell to cell adhesion strength, q=0.1, and strong cell to cell adhesion strength, q=0.9, are superimposed onto the corresponding experimental cell density profile in Figure 5E.
The study showed that the seed bank influenced simulated output during 5 6 years, which is therefore the minimum duration for simulations with an unknown initial seed bank.
Transport properties were computed with NEGF techniques as implemented in TranSIESTA56,61, which allows for simulations with open boundary conditions and multi-terminal configurations.
It is particularly effective for simulations with modest subspace deformations, where it can often verify the absence of self-collisions in constant time.
Even with current computational capabilities that allow for simulations with computational meshes, Reynolds numbers are still limited.
This allows for simulations with a large number of particles (N ∼ 105 106) in reasonable CPU times.
Statistically equivalent virtual polycrystals of the alloy CMSX-4 are created for simulations with the homogenized model.
Large-radii cold fronts, where the field is weaker, are more susceptible to the development of instabilities. Figure 2a: Slices of gas temperature for simulations with different initial plasma $\beta$.
In this paper, we consider how Dynamic Global Vegetation Models (DGVMs), which have been developed for simulations with present day climate, can be used for paleoclimate studies.
Historical baseline (1979 2009) and future (2041 2070) climate scenarios were used for simulations with baseline and future CO2 concentrations of 360 ppmv and 500 ppmv, respectively.
