The rest of permeability tensor elements can be calculated using the same boundary conditions as abovementioned but in other directions.
The rest of permeability tensor elements can be calculated by using the same boundary conditions as abovementioned but in other directions.
Using the same boundary conditions and spherical grains, the self-consistent model is unable to predict this texture transition and only a copper type texture is obtained.
We use the same boundary conditions in the above two problems, i.e., u ( − 40, t ) = u ( 40, t ) = 0. First, for the periodic problem μ = 1, we plot the waveform in Figure 1.
In fact, numerical integrations using the same boundary conditions show that the lowest-order Hermite solution that exhibits such an oscillation has (lambda= 3); for (lambdaleq2), the predicted region for oscillation, (|x| < sqrt{2lambda+ 1}), does not host two critical points of the same kind, and we call such solutions nonoscillatory.
However, compared to using the same boundaries for morning and evening a significant performance improvement (22.8%) was obtained using two different boundaries for morning and evening.
Because we used the same atmospheric boundary conditions for the CTL and CLM experiments, we could not extract the impact of remote SST.
The boundary between the two dB/dt regimes at high latitudes and at low latitudes changes with the extent of the auroral oval, and we can use the same equatorward boundary of the auroral oval used for "caution/warning/emergency" alerts for the boundary between the two regimes.
Once can therefore use the same absorbing boundary conditions in all layers.
Subsequently, the processes were simulated using LS-DYNA3D explicit FE code using the same experimental boundary, loading conditions and the simulation results were compared with the experimental results.
