In order to obtain cost functions of the form w v, v ′ for the computation of Equation 5, we need to compute solutions of the form Rooted-HSA - r (T u v, S u ′ v ′ ) for sub-instances of the input.
The computation of Equation 12 is performed for all the states j, 1≤j≤8, and is iterated for t=2,3,...,T.
Since the exact computation of Equation 25 is not simple in this situation, a well-known approximation is used instead.
A popular method of tsunami numerical simulation is a finite-difference computation of equation of motion for shallow-water waves (momentum conservation) and the equation of continuity (mass conservation) [54].
In fact, the loose coupling between the components of the state vector allows separate and parallel computation of equation sub-systems of much smaller dimension in each cluster heads.
According to the computation of Equation 10, as is shown in Figure 3, when q = 3 m holds, the probability of collision when conflicting location claims are mapped to the same cell is over 99%.
In practice, we can precompute z 1,z 2,…,z δ at items 1 and 2 of Procedure 1 and save them in memory to avoid the algebraic computation of Equation 8 in the hardware.
The computation of Equation 5 using S(E 0 ) obtained from Monte Carlo simulations [22] is given in Figure 7 and shows that contrary to99mTc, the first scattering emission can be reasonably considered as isotropic for90Y.
A precise computation of Equation 24 would require the knowledge of the power delay profile (PDP) to calculate R h =E{h h H }. Since this knowledge can hardly be available at the receiver, we propose to replace R h by an approximation.
