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It can be calculated both from recorded seismic waves and from field measurements of the size of the fault rupture.
It can be calculated in terms of people delayed on their way to work, people injured in accidents, people forced to alter their travel routines.
It can be calculated as follows: .
It can be calculated by Eq. (6).
It can be calculated using Eq. (6).
It can be calculated from Eq. 23.
It can be calculated during information exchange as stated above.
It can be calculated using only classic input and transfer mobilities.
It can be calculated with the following equation: K_{v2} = K_{t} + K_{a} (2).
It can be calculated by the method of next generation matrix given in [32].
It can be calculated that Π > 0 if and only if c m > 15.12.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com