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Notice that the LFP amplitude measured with brief static stimuli (20 ms) is different from the amplitude of LFP frequency components measured with gratings drifting for several seconds (Lashgari et al. 2012).
Every single person with MS is different.
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The priori probability p M k is different when the desired SV lies in a different Category.
While there were no significant differences in scalp distribution between the effect of Word in the 50 150 ms (N1) and in the 150 300 ms (P2) latency bands, the topography of the N400 (300–500 ms) was different from both the N1 and the P2.
Thus, the meaning of the parameter M is different from that in the ordinary M-algorithm.
The basic probability assignment (bpa or m) is different from the classical definition of probability.
The results allow us to explain why the fatigue slope m is different for bending and tension.
Please note that AP-MS is different from the other three methods (BINM, MST and eMST) because that the AP-MS scores are calculated using the raw purification data while the other three methods make predictions based on the AP-MS scores.
Where the coefficients a and m are different for each flow regime and that m = 1 for Darcy flow and m < 1 for pre-Darcy flow.
Note that the amplitude scales for these seismograms (2 × 10−2 m) are different from those for the other stations (2 × 10−4 m).
The RML for the surface layer (0 0.20 m) was different from the root zone (0 0.60 m) and the total active soil profile (0 1.20 m), the latter two having adjacent RMLs.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com