By the same method as used in Theorem 4.1, we can easily prove the following result.
Other Jordan canonical forms in (28) can be treated by the same method as used in Theorem 3.2.
The loading parameterization proposed in this study is the same method as used for classical ocean tide modeling.
However, the estimation of the expected weight is complex, which renders this method, as used presently, less effective.
By the same method as used in the proof of Lemma 3.3, we can demonstrate that (K_{P} I-Q N overline{Omega})) is compact.
Again by using similar method as used in the proof of Theorem 2.8, we can prove that (x^) is the unique fixed point of T. □.
It can be computed by assuming the a priori input to be Gaussian distributed and applying the same method as used for the demapper characteristic T 1.
Using the same method as used in Lemma 3.6, the following inequality holds: biglVert nabla Tdbigl(TDG u bigr bigrVert _{L^{varphi}_{B}} leq C operatorname{diam}(B) Vert u Vert _{L^{varphi}_{sigma B}}.
The RBW simulation with a huge number of test electrons can demonstrate temporal variation of flux distributions in pitch angle and energy using particle weighting method as used in the RB model.
The rest of this paper is organized as follows: In Section 2, we point out some definitions of the Bernstein polynomials and collocation method as used for solving CSFIEs.
This present study adopted a similar method as used by Wang (2014) to study the life-long Chinese learning experience of Chinese language instructors who are native English speakers.
