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The pseudo-bending method (Um and Thurber 1987) was applied to calculate the travel time from a grid node to a station containing its elevation.
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Thus, the main computational effort of the proposed algorithm only consists in solving linear programming problems related to all nodes, which do not grow in size from a grid node to the next node.
Unlike the usual approach, at a given time all the particles from a grid node are simultaneously scattered using the Bernoulli repartition.
Further, switching from a grid topology to a random node topology does not significantly affect the results.
The transfer of input data for the simulation occurs from web portal to grid node selected by the scheduler.
In EEFR, multi-hop routes are formed between neighbor grids from source node to the mobile agent node, which can guarantee the sensory data generated by the farthest node not be lost.
Nakajima and Hasegawa (2007a) applied a travel-time tomography method to arrival-time data from the nationwide seismograph network using grid nodes with a horizontal spacing of 0.2°.
For any of the remaining five ideal grid nodes a subset of local maxima is determined from the remaining local maxima in the scatter plot.
While the 'internal' grid connection involves cost of transformers, secondary MV lines,e LV lines and internal house wiring for connecting households, institutions and other structures within the demand node, the 'external' grid connection entails extending the MV lines from a transformer in the demand node to the closest MV grid network.
Here, online voltage control in the medium-voltage feeders (basing on measurement data from critical grid nodes) by controlling grid components such as tab changer transformers and generation units, the so-called active grid operation [8], can solve the problem of keeping the grid voltage in the defined limits.
The same AGCM output data (2.03 GB) are used as input data for each region simulation, with traffic from the portal to grid nodes.
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Justyna Jupowicz-Kozak
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