Fig. 5From: A straightforward method to compute average stochastic oscillations from data samplesPotential time evolution of the overall azimuthal angle Ï and the polar angle Ξ of the oscillating system. In contrast to the angular coordinate in systems with two species, the polar angle in this trajectory presents no discontinuity. This fact hinders the use of spherical coordinates to assess oscillations in systems with more than two speciesBack to article page