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complex Gaussian entries with zero mean and variance σ H 2. BD is performed with the imperfectly estimated H ^, and therefore the power allocation is determined using the singular values obtained with this estimation error.
In practice, we estimated H using the NSB entropy estimation algorithm (Nemenman et al. 2004), a Bayesian technique using a Dirichlet prior, as described in Supplementary Materials.
In this case, model (11) reduces to y k = H rd D k E H sr S 0 + V k, k = 1, …, K, (64) Figure 3 NMSE of estimated H sr and H rd. Proposed estimators (TALS and KRLS) vs. conventional LS estimator.
Estimated H parameters usually fall between 0 and 1 in agreement with physical theories (Geist 2002; Mai and Beroza 2002).
Figure 4 Map of estimated H 2 O content in relatively primitive basalt from the Northeast Japan and Izu arcs.
Note that the upper limit set for the estimated H s is greater than the maximum value of H s measured by the buoy for both platforms (see Figure 2).
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A total of 18 MVT were found amongst 25 randomly sampled colonies, and the estimated H-1 2.5 H-1 2.5ion population of MVT was 0.69 (Table 1).
MMSE estimation is performed to estimate h i, m.
The channel estimation problem is to estimate H from the observation Y.
To assess the combination Method - Model to estimate H R t), the bias and the RMSE of the estimations presented above were calculated.
The BS estimates h k 's using the minimum mean square error (MMSE) estimator.
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CEO of Professional Science Editing for Scientists @ prosciediting.com