Sentence examples for epoch day from inspiring English sources

To examine a response of scintillation and to propose a method of scintillation forecasting relative to arrival time of CIRs and ICMEs, Prikryl et al. (2012) focused on the cusp stations in Cambridge Bay and Taloyoak that showed steep increases in scintillation occurrence on the zero epoch day tapering off a few days later.

The lowest scintillation occurrences and lowest probabilities are found for epoch day -2, i.e., 2 days before HSS/CIR arrival.

It is noted that the lowest occurrences (Figures 3a and 4) and the lowest probabilities (Figures 7a and 8b) are observed 2 days before HSS/CIR arrivals, i.e., on epoch day -2. Figure 8 Same as Figure 7 a,b but showing the cumulative PDFs for the nightside auroral zone.

For each epoch day, the phase scintillation occurrence and mean number of cycle slips maximized in the cusp and extended into the polar cap with the grand maximum occurring on the epoch day 0.

In the 'cusp', while the PDFs just after the arrival of an event (epoch day 0) are very similar for non-MC (Figure 10c) and MC (Figure 10d) events, the 'background' PDFs before and a few days after the epoch day 0 are lower for the MC subset (Figure 10d).

However, in all instances, both in the cusp and in the auroral zone, the highest probability of phase scintillation occurrence is on epoch day 0, i.e., just after the arrival of CIRs or ICMEs.

The scintillation occurrence (probability) is strongly affected by the variability of the magnetic field.In Figure 7a,b, the overall PDFs are shown from -6 to +6 epoch days stepped by 1-day intervals for HSS/CIRs and ICMEs, respectively.

Frederick Engels called the vote "an epoch-making day" and a St Louis labor leader predicted it would become "the battle cry for all the enslaved toilers from the Atlantic to the Pacific".

A coastal evolution model is applied to simulate the impact of different hypothetical mega-nourishment interventions to assess their impacts' over 3 shoreline management planning epochs: present-day (0 20 years), medium-term (20 50 years) and long-term (50 100 years).

We averaged data recorded at the same epoch (within 1 day) in each bin, which provided values at the same geographic location at different epochs and different altitudes.

If however the difference between the experiment observation time and the Bulletin A epoch exceeds 1 day, we quickly see that the polar motion uncertainty starts to dominate the UT1-UTC estimate accuracy.