Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results

The forecasting of lava flow paths is a complex problem in which temperature, rheology and flux-rate all vary with space and time. The problem is more difficult to solve when lava runs down a real topography, considering that the relations between characteristic parameters of flow are typically nonl...

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Main Authors: C. Del Negro, L. Fortuna, A. Vicari
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/12/505/2005/npg-12-505-2005.pdf
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spelling doaj-9145c0dd50a74cfb87ffffb249c7883b2020-11-24T22:04:52ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462005-01-01124505513Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary resultsC. Del NegroL. FortunaA. VicariA. VicariThe forecasting of lava flow paths is a complex problem in which temperature, rheology and flux-rate all vary with space and time. The problem is more difficult to solve when lava runs down a real topography, considering that the relations between characteristic parameters of flow are typically nonlinear. An alternative approach to this problem that does not use standard differential equation methods is Cellular Nonlinear Networks (CNNs). The CNN paradigm is a natural and flexible framework for describing locally interconnected, simple, dynamic systems that have a lattice-like structure. They consist of arrays of essentially simple, nonlinearly coupled dynamic circuits containing linear and non-linear elements able to process large amounts of information in real time. Two different approaches have been implemented in simulating some lava flows. Firstly, a typical technique of the CNNs to analyze spatio-temporal phenomena (as Autowaves) in 2-D and in 3-D has been utilized. Secondly, the CNNs have been used as solvers of partial differential equations of the Navier-Stokes treatment of Newtonian flow.http://www.nonlin-processes-geophys.net/12/505/2005/npg-12-505-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Del Negro
L. Fortuna
A. Vicari
A. Vicari
spellingShingle C. Del Negro
L. Fortuna
A. Vicari
A. Vicari
Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
Nonlinear Processes in Geophysics
author_facet C. Del Negro
L. Fortuna
A. Vicari
A. Vicari
author_sort C. Del Negro
title Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
title_short Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
title_full Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
title_fullStr Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
title_full_unstemmed Modelling lava flows by Cellular Nonlinear Networks (CNN): preliminary results
title_sort modelling lava flows by cellular nonlinear networks (cnn): preliminary results
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2005-01-01
description The forecasting of lava flow paths is a complex problem in which temperature, rheology and flux-rate all vary with space and time. The problem is more difficult to solve when lava runs down a real topography, considering that the relations between characteristic parameters of flow are typically nonlinear. An alternative approach to this problem that does not use standard differential equation methods is Cellular Nonlinear Networks (CNNs). The CNN paradigm is a natural and flexible framework for describing locally interconnected, simple, dynamic systems that have a lattice-like structure. They consist of arrays of essentially simple, nonlinearly coupled dynamic circuits containing linear and non-linear elements able to process large amounts of information in real time. Two different approaches have been implemented in simulating some lava flows. Firstly, a typical technique of the CNNs to analyze spatio-temporal phenomena (as Autowaves) in 2-D and in 3-D has been utilized. Secondly, the CNNs have been used as solvers of partial differential equations of the Navier-Stokes treatment of Newtonian flow.
url http://www.nonlin-processes-geophys.net/12/505/2005/npg-12-505-2005.pdf
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