Articles | Volume 12, issue 4
Nonlin. Processes Geophys., 12, 505–513, 2005
https://doi.org/10.5194/npg-12-505-2005
Nonlin. Processes Geophys., 12, 505–513, 2005
https://doi.org/10.5194/npg-12-505-2005

  19 May 2005

19 May 2005

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

C. Del Negro1, L. Fortuna2, and A. Vicari1,2 C. Del Negro et al.
  • 1Istituto Nazionale di Geofisica e Vulcanologia – Sezione di Catania, Italy
  • 2Università di Catania – Dipartimento di Ingegneria Elettrica Elettronica e dei Sistemi, Italy

Abstract. 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.

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