On spectra of weighted graphs of order ≤5

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A new processing methodology of wind profiler Doppler spectra called UBWPP (Method 2) has been described, addressing the computation of horizontal and vertical wind components,

In the case of non orientable surfaces, 8,9 , the authors introduced graphs with pairs of weights on the vertices, associated to stable maps from closed surfaces to the

where  AL←M and  R←M are the effect of M on ADG AL and ADG R , respectively; b is the vector of systematic effects, with incidence matrix X , which included the effects of

The emission spectra of a single QD are shown in Figure 5.7 for different excitation power P. The enlargement factors are indicated and spectra are shifted vertically for clarity.

In the previous sections we have shown how astronomical alignments and solar hierophanies – with a common interest in the solstices − were substantiated in the

These graphs are the nihilation matrix and the negative initial digraph respectively, and contain information about potential dangling edges (i.e. edges that would become dangling

Comparison of the experimental Ni K-edge XANES spectra for 1 Eq-ML of NiO on SiO 2 and MgO and the theoretical spectra calculated for both a NiO cluster (solid line) and for a