Errors are not estimated for each individual source, but instead they are, in total, estimated to be 35%, 30 %, 60, and 60% andN60% WIDE-S, WIDE-L, atd N600, respectively (Yamamura et al., 2009).
Errors are not estimated for each individual source, but instead they are, in total, estimated to be 35%, 30 %, 60, and 60% and60%μm, 90 μm, 140 μm, atd 165 μm, respectively (Yamamura et al., 2010).
The flux errors are not estimated for each individual source, but instead they are estimated, in total, to be 35%, 30 %, 60, and 60% and60%μm, 90 μm, 140 μm, atd 165 μm, respectively (Yamamura et al., 2010).
Thus, only one dipole strength should be estimated for each dipole source.
The main task in the first step is to estimate the electric angle γ, whereas in the second step, ϕ related to γ is estimated for each near-field source.
Table 4. Sediment delivered to the stream network (tonnes per year [tons per year]) is estimated for each management plan, study period and source area.
The strength of the fixed-location sources was estimated for each time-instant of the evoked response applying the linear inverse solution using a cortical loose orientation constraint [114].
Daily contributions of PM2.5 sources were estimated for each monitoring location using positive matrix factorization (PMF) (Bell et al. 2010; Norris et al. 2008; Paatero and Tapper 1994).
Ideally, the dose, time pattern, and frequencies (wavelengths) of exposure from all key sources should be estimated for each individual in the study.
Sources spectral densities were estimated for each band by means of standardized low-resolution brain electromagnetic tomography (sLORETA) in the frequency domain25,26 for each 2 s epoch using sLORETA free software26.
