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This results in a normalized time scale τ = f t with arbitrary units that is used throughout this publication.
In a normalized time scale (Fig. 4B), the voltage responses of photoreceptors and LMCs showed striking similarities at different playback velocities of stimulation.
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The superposition used the 1-h time-resolution bins in the normalized time period.
In each normalized time block, the WET is performed in the first β fraction of time.
The equilibration time of Eq. (35) is calculated to be 1.5 in the normalized time.
Here we estimate a variation in the stressing rate in the NKTZ from the spatial variation in the normalized time delay of shear wave splitting.
The observed variation in the normalized time delay can, therefore, be interpreted to reflect the variation in the stressing rate in the NKTZ.
Following Hiramatsu et al. (2010), we adopt here RSC SP = 880/(MPa) from the change in normalized time delays caused by the step-wise static stress change of a moderate size earthquake (Saiga et al. 2003; Hiramatsu et al. 2005) and T C = 2 years from the recovery of crack conditions to a step-wise static stress change (Hiramatsu et al. 2005; Sugaya et al. 2009).
At least, more than 10 in normalized time seems necessary for local equilibration.
Figure 9 Comparison of 802.11p and UWB PDP trends in normalized time scale.
In Fig. 3, normalized time correlation function data at a scattering angle of 90o for a high and a low concentration of MHEC- g-PNIPAAM and MHEC- g-PNIPAAM at various temperatures are depicted in form of semilogarithmic plots.
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