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simulated results
Finally, to analyze the impacts of the fiber nonlinear effects and PMD on the optical communication system, the simulated results of an 8×40 Gbit/s DWDM system are discussed under different conditions respectively.
      
The simulated results show that FSS may operate in different bands and especially generate a large reduction in the resonant frequency for a fixed unit cell size through different loadings.
      
Practical circuits are fabricated, and the measured results agree well with the simulated results.
      
The simulated results indicate that a steplike magnetization behavior is very sensitive to the concentration of AFM bonds.
      
Numerical values of interaction parameters were obtained by fitting simulated results to refined experimental data.
      
The simulated results are compared with previous experimental findings.
      
Simulated results are presented and analyzed, showing that the proposed technique has an excellent performance even when the signal-to-noise ratio is very low (-23 dB).
      
Previously, the smallness of the residual arising from substitution of simulated results into the initial system of equations is demonstrated and the residual's dependence on the number of reference functions and supercriticality is considered.
      
The simulated results that match the experiments well show the validity of the proposed domain-switching model.
      
Simulated results reproduced the morphology transitions of deep cell to shallow cell and shallow cell to plane front.
      
On the basis of simulated results of temperature and geopotential height patterns we emphatically discuss the effects of the topography and the heating of the Qinghai-Xizang Platcau.
      
The simulated results show that (1) the front of the lake breeze progresses inland faster in the late afternoon than at the fully developed stage; and (2) the lake breeze and land breeze have larger, extension offshore than inland.
      
A comparison of the simulated results with experimental data shows that high SO2 concentration centres correspond to low pH centres.
      
Moreover, the numerically simulated results show that the above-mentioned EU-pattern anomalies of circulation are due to the propagations of planetary wave train.
      
The simulated results with either of the two negative temperatures are reasonably consistent with those from the statistical theory of turbulence.
      
Our purpose is to test the effciency of TTT in higher dimensional model and the sensitivity of simulated results to the TTT parameters.
      
The simulated results suggested that the sensible heat flux was closely proportional to the square of wind speed in the surface layer.
      
The simulated results are also compared with the reanalysis data.
      
The simulated results show that the slope parameter b and the intercept d of the meteoric water line (MWL), δD = bδ18O+d, in wet adiabatic cooling are both greater than those in isobaric cooling.
      
However, there are still some differences in the simulated results compared with the reanalysis data.
      
 

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