DocumentCode
2274437
Title
Volcano monitoring via fractal modeling of lava flows
Author
Martino, Gerardo Di ; Iodice, Antonio ; Riccio, Daniele ; Ruello, Giuseppe
Author_Institution
Dipt. di Ing. Elettron. e delle Telecomun., Univ. di Napoli "Federico II", Naples, Italy
fYear
2008
fDate
11-14 Nov. 2008
Firstpage
1
Lastpage
5
Abstract
In this paper use is made of fractal models for the development of a processing chain devoted to volcano monitoring. In particular, we present new models for the characterization of microwave images of fractal surfaces and we show how these models can account for the presence of different types of lava flows on these images.The imaged surfaces are modeled as fractional Brownian motion (fBm) stochastic processes. First of all, we show how the radar image relevant to an fBm can be linked to an associated fractional Gaussian noise (fGn) process. Different types of lava flow surfaces are simulated and their image spectra are analyzed and compared. Finally, a case study is presented. The area of interest is the Vesuvio volcano close to Naples, Italy. Simulated results, showing the possibility to discriminate different types of lava, are provided.
Keywords
Brownian motion; Gaussian noise; microwave imaging; remote sensing by radar; stochastic processes; synthetic aperture radar; volcanology; Italy; Naples; TerraSAR-X data; Vesuvio volcano; fBm stochastic process; fGn process; fractional Brownian motion; fractional Gaussian noise; lava flow fractal modeling; microwave imaging; radar image; synthetic aperture radar; volcano monitoring; Fractals; Image analysis; Image resolution; Image sensors; Layout; Monitoring; Performance analysis; Radar imaging; Telecommunications; Volcanoes;
fLanguage
English
Publisher
ieee
Conference_Titel
Use of Remote Sensing Techniques for Monitoring Volcanoes and Seismogenic Areas, 2008. USEReST 2008. Second Workshop on
Conference_Location
Naples
Print_ISBN
978-1-4244-2546-4
Electronic_ISBN
978-1-4244-2547-1
Type
conf
DOI
10.1109/USEREST.2008.4740342
Filename
4740342
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