Giuseppe Roberto Tomasicchio

Prof. Dr. Giuseppe Roberto Tomasicchio

Department of Engineering, University of Salento, 73100 Lecce – Italy
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orcid

Research Focus & Metrics

Academic Career Length

34Years (1993-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 June 2014 in Coastal Engineering
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Journal Article
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GSG. Salvadori
G. Salvadori
Giuseppe Roberto TomasicchioGiuseppe Roberto Tomasicchio
Giuseppe Roberto Tomasicchio
Felice D'AlessandroFelice D'Alessandro
Felice D'Alessandro

10 September 2018 in Water
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Journal Article
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Daniela PantusaDaniela Pantusa
Daniela Pantusa
Felice D'AlessandroFelice D'Alessandro
Felice D'Alessandro
LRLUIGIA RIEFOLO
LUIGIA RIEFOLO
FPFrancesca Principato
Francesca Principato
Giuseppe Roberto TomasicchioGiuseppe Roberto Tomasicchio
Giuseppe Roberto Tomasicchio
The coastal vulnerability index (CVI) is a popular index in literature to assess the coastal vulnerability of climate change. The present paper proposes a CVI formulation to make it suitable for the Mediterranean coasts; the formulation considers ten variables divided into three typological groups: geological; physical process and vegetation. In particular, the geological variables are: geomorphology; shoreline erosion/accretion rates; coastal slope; emerged beach width and dune width. The physical process variables are relative sea-level change; mean significant wave height and mean tide range. The vegetation variables are width of vegetation behind the beach and posidonia oceanica. The first application of the proposed index was carried out for a stretch of the Apulia region coast, in the south of Italy; this application allowed to (i) identify the transects most vulnerable to sea level rise, storm surges and waves action and (ii) consider the usefulness of the index as a tool for orientation in planning strategies. For the case study presented in this work, the most influential variables in determining CVI are dune width and geomorphology. The transects that present a very high vulnerability are characterized by sandy and narrow beaches (without dunes and vegetation) and by the absence of Posidonia oceanica.

1 January 2015 in Coastal Engineering
Verified
Journal Article
Closed access
GSG. Salvadori
G. Salvadori
FDFabrizio Durante
Fabrizio Durante
Giuseppe Roberto TomasicchioGiuseppe Roberto Tomasicchio
Giuseppe Roberto Tomasicchio
Felice D'AlessandroFelice D'Alessandro
Felice D'Alessandro

1 January 2013 in Coastal Engineering
Verified
Journal Article
Closed access
Giuseppe Roberto TomasicchioGiuseppe Roberto Tomasicchio
Giuseppe Roberto Tomasicchio
Felice D'AlessandroFelice D'Alessandro
Felice D'Alessandro
GBGiuseppe Barbaro
Giuseppe Barbaro
Giovanni MalaraGiovanni Malara
Giovanni Malara

9 September 2019 in Water Resources Research
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Pierfranco CostabilePierfranco Costabile
Pierfranco Costabile
Costanzo CarmelinaCostanzo Carmelina
Costanzo Carmelina
Samuele De BartoloSamuele De Bartolo
Samuele De Bartolo
Fabiola GangiFabiola Gangi
Fabiola Gangi
Francesco MacchioneFrancesco Macchione
Francesco Macchione
Giuseppe Roberto TomasicchioGiuseppe Roberto Tomasicchio
Giuseppe Roberto Tomasicchio
This paper is focused on the contribution that the two‐dimensional Shallow Water Equations could provide in respect to the fields of research devoted to the river networks analysis. The novelty introduced in this work is represented, in particular, by the hydraulic characterization of the river drainage networks, starting from flow patterns simulated by the two‐dimensional Shallow Water Equations on high‐resolution digital elevation model (DEM) through the analysis of water depths flowing down the hillslopes, channelized in both the main river and in all the tributaries or stored in small depressions. The first finding of this research is the determination of scaling laws that describe the relations between the water depth threshold, used to identify the network cells, and a dimensionless area, related to the total area of the network cells themselves. The observed bimodal scaling behavior has been considered as representative of the flow patterns belonging to the channel networks (CN) and hillslope plus channel networks (HCN), the physical and geomorphological interpretation of which has been provided from a multifractal point of view. In particular, the analysis of the multifractal spectra highlights significant variations in the multifractal signatures, between the CN and the HCN structures, leading to the proposal of a novel criterion for channels heads detection that has provided encouraging predictions of field observations.

17 June 2021 in Energies
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SRSara Russo
Sara Russo
PCPasquale Contestabile
Pasquale Contestabile
ABAndrea Bardazzi
Andrea Bardazzi
ELElisa LEONE
Elisa LEONE
Gregorio IglesiasGregorio Iglesias
Gregorio Iglesias
Diego VicinanzaDiego Vicinanza
Diego Vicinanza
New large-scale laboratory data are presented on a physical model of a spar buoy wind turbine with angular motion of control surfaces implemented (pitch control). The peculiarity of this type of rotating blade represents an essential aspect when studying floating offshore wind structures. Experiments were designed specifically to compare different operational environmental conditions in terms of wave steepness and wind speed. Results discussed here were derived from an analysis of only a part of the whole dataset. Consistent with recent small-scale experiments, data clearly show that the waves contributed to most of the model motions and mooring loads. A significant nonlinear behavior for sway, roll and yaw has been detected, whereas an increase in the wave period makes the wind speed less influential for surge, heave and pitch. In general, as the steepness increases, the oscillations decrease. However, higher wind speed does not mean greater platform motions. Data also indicate a significant role of the blade rotation in the turbine thrust, nacelle dynamic forces and power in six degrees of freedom. Certain pairs of wind speed-wave steepness are particularly unfavorable, since the first harmonic of the rotor (coupled to the first wave harmonic) causes the thrust force to be larger than that in more energetic sea states. The experiments suggest that the inclusion of pitch-controlled, variable-speed blades in physical (and numerical) tests on such types of structures is crucial, highlighting the importance of pitch motion as an important design factor.