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The characteristics of an infrasonic wave induced by a small volumetric change at the ground surface are given by Yamasato (1998) and shown in Figure 11: V = r p o ρ τ 2 = 4 r p o ρ Δ t 2. where r is the distance from the source to the receiver, ρ is the density of the air, po is the maximum negative amplitude of the rarefaction phase, τ is the rise time of the downlift, and Δt is the pulse width.
The MMN peak was defined as the maximum negative amplitude between 150 and 250 ms at electrode FCz.
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Maximum amplitude measures the maximum positive or negative amplitude of a trace and potential low velocity medium within a time or depth window.
We defined latency and amplitude of summating potential at the initial negative deflection arising from baseline while compound action potential peak amplitude was measured at maximum negative potential (with respect to baseline).
As stated in the previous sub-section, the amplitude of the MI is defined as ΔH = H th2) − H th1), where th1 is the onset time of SI and th2 is the time when the amplitude of the SI attains its maximum negative value.
As the distance increases, the time cross-correlation curve starts at very low (even negative) amplitude and then increases with a maximum in amplitude which is due to the average transit time (diffusive or not) between the two locations (e.g. pCF 5) curve).
Amplitudes and latencies of the photopic ERG b-wave were measured at the maximum negative and positive peaks of the recordings with respect to the baseline before the stimulation.
Maximum flooding surface 2 and maximum flooding surface 3 correspond to positive amplitudes denoted by peak (blue color), while MFS 1 corresponds to negative amplitude denoted by trough (red color) (Fig. 7).
Amplitudes and latencies of the scotopic ERG a- and b-waves were measured at the maximum negative and positive peaks of the recordings with respect to the baseline before the stimulation.
The negative amplitude of a.f.
The received electrical signal, however, can assume negative amplitude values.
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