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This model is validated using the data sets from the corresponding stations during 1965 1966, and the results show larger uncertainties than the calibrating model.
Figure 8b shows the MLT variation of the contribution at corresponding stations due to the magnetopause currents using the T01 model for SW and IMF conditions identical to those occurred during the presently studied case, and Figure 8c shows the MLT profile of the residual field in the H component after subtracting the contribution from the magnetopause currents from the observed MI amplitude.
The observed peak velocities for the transverse components are greater than 4.0 and 2.5 cm/s at the stations 200 and 400 km away from the fault plane whereas the predicted values from the empirical relation are around 1.0 and 0.2 cm/s for the corresponding stations.
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The interlocking table has been created for the corresponding station, and the accuracy of it has been checked it out by the introduced models via NuSMV.
The summation in parenthesis is the time required for the corresponding station to acknowledge the poll by returning a combined Data/CF-ACK frame.
Note that these events are plotted at the same epicentral distances as the recording Hi-net stations, at times corresponding to their P-wave arrival at the corresponding station.
The 'station_distances' database contains all possible segment identities and the corresponding station-to-station distances, ordered as a continuous journey that visits every station in the network in each direction (repeating sections of the network if necessary).
Once the information is retrieved, all EOLPs are shipped either to station 1 for disassembly or, if it only needs one component, it is sent to its corresponding station.
Then, the station H -component variations are normalized to the difference between the H -component values and the mean local midnight values for the five quietest days, providing the Δ H for that corresponding station.
Stations positioned at each region, STS-1, STS-2, and STS-3 communicate with their corresponding wired stations two hops away from them.
Figure 1 shows the epicenters of these aftershocks and the locations of the corresponding triggered stations.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com