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FIGURE 19 Simulation of mean surface elevation induced FIGURE 21 Simulation of nearshore circulation currents induced
by morphological waves at Cala Azzurra by morphological waves at Cala Azzurra
FIGURE 20 Simulation of mean surface elevation induced FIGURE 22 Simulation of nearshore circulation currents induced
by morphological waves at Lido Burrone by morphological waves at Lido Burrone
4. In general, more intense coastal dynamics and investigated by means of measures, experimental and
hydrodynamic conditions were observed at Cala mathematical model studies, including the description
Azzurra compared to Lido Burrone. of coastal hydraulics and sediment dynamics.
The results are interesting not only for the purpose of $FNQRZOHGJHPHQWV
the project, but also because they can be considered as Hydrographic surveys and field activities were
representative of the typical morphology and dynamics performed in cooperation with the Area Marina Protetta
of the pocket beaches, that is a key issue in coastal Isole Egadi Management Authority. The contribution by
sciences. Stefano Donati (director), Daniela Sammartano, Monica
Further studies could be suggested in order to better Russo, Giuseppe Cammareri and Alessandro Agate is
investigate the possible causes for the evidences gratefully acknowledged. O
observed in field activities. In particular, assuming
that the Posidonia oceanica coverage has undoubtedly Francesco Pasanisi, Carlo Tebano, Sergio Grauso
positive effects on sea bottom stability, its role could be ENEA, Sustainable Territorial and Production Systems Department
58 EAI Energia, Ambiente e Innovazione 4/2015
