First we introduced the equations for calculating the Group Error Rate (GER).
Moreover, the outcomes of apoptosis and necrosis can be explained without this assumption, by deleting equation 33 (Table 1) which models level 2 pore opening via sustained [Ca2+]i increase and by introducing the equation PMCht = PMCht+1 prolonging the opening of plasma membrane channels over the simulation time.
In Section 2, we introduce the equations governing the atmospheric circulation with magnetic field and also give the bifurcation theory.
In the first part we will introduce the equations which govern the spatial and temporal behavior of τ (r, t ) in the presence of PT excitation, thermal diffusion and flow-dependent heat convection.
We have recently introduced the map equation to simplify and highlight important structures with respect to the dynamics on networks.
He worked on mathematical models for weather prediction and introduced the Rossby equations, which were used in 1950 with an advanced electronic computer to forecast the weather.
This chapter has introduced the AGMA equations for modelling bending and contact stresses in spur gears.
Recently, Chepzhov and Vishik [9] introduced the atmospheric equations considered in this paper.
In the present study, firstly, we introduced the Moens-Korteweg equation and its deduced equation for investigating the relationship of PTT and BP.
In particular, Rassias [11] introduced the quartic functional equation.
