Fig. 3 Illustration of multi-path CIR in Gaussian low-pass filter channel model (upper) and after pre-ltering (lower).
The present element, together with the eight-node isoparametric plate element based on a first order shear deformation theory used to model the upper and lower adherends, is found to be effective in solving free vibration problems of adhesively bonded laminated lap-joints.
Fig. 8 Variation of night-time electron densities according to the original and the modified IMAZ model (upper panel), and the resulting simulated integral absorption (lower panel).
Fig. 9 Diurnal variation of electron densities at various heights for 3 dB riometer absorption (median conditions, mid-April) according to the original and the extended IMAZ model (upper panel), and the corresponding integral absorption (lower panel).
Several radiation belt models currently use models of upper and lower band chorus defined using the local electron gyrofrequency [ Varotsou et al., 2005; Fok et al., 2008; Albert et al., 2009; Glauert et al., 2014] and do not include wave power below 0.1 fce.
Elastic brittle fracture model and ideal elastoplastic model are special cases of this model when upper and lower limit of distribution interval are equal.
The two-dimensional series and parallel models provide upper and lower bounds of the effective diffusion coefficient, respectively, whereas the three-dimensional model provides the accurate effective diffusion coefficient.
According to the two-part model, the upper and lower boundaries of the predicted EQ-5D are lower than the OLS models.
The earth crust has a two-layer structure in our model, representing upper and lower crusts.
In this model, electrodes (upper and lower) and plasma are divided into small elements of length ΔX.
