  We show that the clustering coefficient, a standard measure in network
theory, when applied to flow networks, i.e. graph representations of fluid
flows in which links between nodes represent fluid transport between spatial
regions, identifies approximate locations of periodic trajectories in the flow
system. This is true for steady flows and for periodic ones in which the time
interval $\tau$ used to construct the network is the period of the flow or a
multiple of it. In other situations the clustering coefficient still identifies
cyclic motion between regions of the fluid. Besides the fluid context, these
ideas apply equally well to general dynamical systems. By varying the value of
$\tau$ used to construct the network, a kind of spectroscopy can be performed
so that the observation of high values of mean clustering at a value of $\tau$
reveals the presence of periodic orbits of period $3\tau$ which impact phase
space significantly. These results are illustrated with examples of increasing
complexity, namely a steady and a periodically perturbed model two-dimensional
fluid flow, the three-dimensional Lorenz system, and the turbulent surface flow
obtained from a numerical model of circulation in the Mediterranean sea.
