http://www.cnr.it/ontology/cnr/individuo/prodotto/ID66812
Simulating debris flows through a hexagonal cellular automata model: SCIDDICA S3-hex (Articolo in rivista)
- Type
- Label
- Simulating debris flows through a hexagonal cellular automata model: SCIDDICA S3-hex (Articolo in rivista) (literal)
- Anno
- 2003-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.5194/nhess-3-545-2003 (literal)
- Alternative label
D'AMBROSIO D. (1), DI GREGORIO S. (1) & IOVINE G. (2) (2003)
Simulating debris flows through a hexagonal cellular automata model: SCIDDICA S3-hex
in Natural hazards and earth system sciences (Print); Copernicus GmbH, Katlenburg-Lindau (Germania)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- D'AMBROSIO D. (1), DI GREGORIO S. (1) & IOVINE G. (2) (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- Copernicus GmbH (Copernicus Publications), ISSN: 1561-8633.
Scopus: 2-s2.0-1642332457
SCImago SJR (2003) = 0,000 - Subject Category: Geology: Q3
DOI: 10.5194/nhess-3-545-2003 - URL: http://www.nat-hazards-earth-syst-sci.net/3/545/2003/nhess-3-545-2003.html
G-Scholar: http://scholar.google.it/scholar?oi=bibs&hl=it&cluster=16513911153288148984 - http://scholar.google.it/scholar?oi=bibs&hl=it&cluster=3167195022121070416
Numero di citazioni = 57 al 26 ago 2013 - fonte: G-Scholar
Numero di citazioni = 39 al 21 ott. 2013 - fonte: Scopus
Impact Factor: 1.751 (2012) cfr. Journal Citation Reports®, Published by Thomson Reuters - ISI WoS
SCImago SJR (2012) = 0,889 - Subject Category: Geology: Q1 (literal)
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- 1) Unical-Dip. Matematica
2) CNR-IRPI UOS di Cosenza (literal)
- Titolo
- Simulating debris flows through a hexagonal cellular automata model: SCIDDICA S3-hex (literal)
- Abstract
- Cellular Automata (CA) represent a formal frame
for dynamical systems, which evolve on the base of local
interactions. Some types of landslide, such as debris flows,
match well this requirement.
The latest hexagonal release (S3-hex) of the deterministic
model SCIDDICA, specifically developed for simulating
debris flows, is described. For CA simulation purposes, landslides
can be viewed as a dynamical system, subdivided into
elementary parts, whose state evolves exclusively as a consequence
of local interactions within a spatial and temporal
discretum. Space is the world of the CA, here constituted
by hexagonal cells. The attributes of each cell (\"substates\")
describe physical characteristics. For computational reasons,
the natural phenomenon is \"decomposed\" into a number of
elementary processes, whose proper composition makes up
the \"transition function\" of the CA. By simultaneously applying
this function to all the cells, the evolution of the phenomenon
can be simulated in terms of modifications of the
substates.
SCIDDICA S3-hex exhibits a great flexibility in modelling
debris flows. With respect to the previous releases of the
model, the mechanism of progressive erosion of the soil
cover has been added to the transition function. Considered
substates are: altitude; thickness and energy of landslide debris;
depth of erodable soil cover; debris outflows. Considered
elementary processes are: mobilisation triggering and
effect (T1), debris outflows (I1), update of landslide debris
thickness and energy (I2), and energy loss (T2).
Simulations of real debris flows, occurred in Campania
(Southern Italy) in May 1998 (Sarno) and December 1999
(San Martino V.C. and Cervinara), have been performed for
model calibration purposes; some examples of analysis are
briefly described. Possible applications of the method are:
risk mapping, also based on a statistical approach; evaluating
the effects of mitigation actions (e.g. stream deviations,
topographic alterations, channelling, embankments, bridges,
etc.) on flow development. (literal)
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