A proper understanding of sediment transport dynamics, critically
including resuspension and deposition processes of suspended sediments,
is key to the morphodynamics of shallow tidal environments. Aiming to
account for deposition mechanics in a synthetic theoretical framework
introduced to model erosion dynamics, here we investigated suspended
sediment dynamics. A complete spatial and temporal coverage of suspended
sediment concentration (SSC) required to effectively characterize
resuspension events is hardly available through observation alone, even
combining point measurements and satellite images, but it can be
retrieved by properly calibrated and tested numerical models. We
analyzed one-year-long time series of SSC computed by a bi-dimensional,
finite-element model in six historical configurations of the Venice
Lagoon in the last four centuries. Following the peak-over-threshold
theory, we statistically characterized suspended sediment dynamics by
analyzing interarrival times, intensities and durations of
over-threshold SSC events. Our results confirm that, as for erosion
events, SSC can be modeled as a marked Poisson process in the intertidal
flats for all the considered historical configurations of the Venice
Lagoon because exponentially distributed random variables well describe
interarrival times, intensity and duration of over-threshold
events. Moreover, interarrival times, intensity and duration describing
local erosion and over-threshold SSC events are highly related, although
not identical because of the non-local dynamics of suspended sediment
transport related to advection and dispersion processes. Owing to this
statistical characterization of SSC events, it is possible to generate
synthetic, yet realistic, time series of SSC for the long-term modeling
of shallow tidal environments.