<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>8</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/nhess-8-369-2008</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/8/369/2008/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/8/369/2008/nhess-8-369-2008.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/8/369/2008/nhess-8-369-2008.pdf</fulltext_pdf>
	<start_page>369</start_page>
	<end_page>376</end_page>
	<publication_date>2008-04-24</publication_date>
	<article_title content_type="html">Automatic estimation of optimal autoregressive filters for the analysis of volcanic seismic activity</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>P. Lesage</name>
			<email>lesage@univ-savoie.fr</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Géophysique Interne et Tectonophysique, CNRS, IRD: R157, Université de Savoie, 73376 Le Bourget-du-Lac Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">Instituto de Geofísica, Universidad Nacional Autónoma de México, Mexico, D.F., Mexico</affiliation>
	</affiliations>
	<abstract content_type="html">Long-period (LP) events observed on volcanoes provide important information
for volcano monitoring and for studying the physical processes in magmatic
and hydrothermal systems. Of all the methods used to analyse this kind of
seismicity, autoregressive (AR) modelling is particularly valuable, as it
produces precise estimations of the frequencies and quality factors of the
spectral peaks that are generated by resonance effects at seismic sources
and, via deconvolution of the observed record, it allows the excitation
function of the resonator to be determined. However, with AR modelling
methods it is difficult to determine the order of the AR filter that will
yield the best model of the signal. This note presents an algorithm to
overcome this problem, together with some examples of applications. The
approach described uses the kurtosis (fourth order cumulant) of the
deconvolved signal to provide an objective criterion for selecting the
filter order. This approach allows the partial automation of the AR analysis
and thus provides interesting possibilities for improving volcano monitoring
methods.</abstract>
	<references>
		<reference numeration="1" content_type="text">Adnet, C.: Unification des méthodes d&apos;analyse spectrale (Fourier et haute résolution) en vue de la réalisation d&apos;un système expert d&apos;aide à l&apos;analyse. Ph.D. Thesis, INPG, Grenoble, France, 1990. </reference>
		<reference numeration="2" content_type="text">Brenguier, F., Shapiro, N. M., Campillo, M. et al.: Towards forecasting volcanic eruptions using seismic noise, Nature Geoscience, 1, 126&amp;ndash;130, doi:10.1038/ngeo104, 2008. </reference>
		<reference numeration="3" content_type="text">Carniel, R., Di Cecca, M. and Rouland, D.: Ambrym, Vanuatu (July&amp;ndash;August 2000): spectral and dynamical transitions on the hours-to-days timescale. J. Volcanol, Geotherm. Res., 128, 1&amp;ndash;13, doi:10.1016/S0377-0273(03)00243-9, 2003. </reference>
		<reference numeration="4" content_type="text">Chouet, B.: Dynamics of a fluid-driven crack in three dimensions by the finite difference method, J. Geophys. Res., 91(B14), 13 967&amp;ndash;13 992, 1986. </reference>
		<reference numeration="5" content_type="text">Chouet, B.: A seismic model for the source of long-period events and harmonic tremor, in: Volcanic seismology, edited by: P. Gasparini, R. Scarpa, and K. Aki, Berlin, 133&amp;ndash;156, 1992. </reference>
		<reference numeration="6" content_type="text">Chouet, B.: Long-period volcano seismicity: its source and use in eruption forecasting, Nature, 380, 309&amp;ndash;316, 1996a. </reference>
		<reference numeration="7" content_type="text">Chouet, B.: New methods and future trends in seismological volcano monitoring, In: Monitoring and mitigation of volcano hazards, edited by: R. Scarpa and R. I. Tilling, 23&amp;ndash;97, 1996b. </reference>
		<reference numeration="8" content_type="text">Chouet, B., Sacorrotti, G., Dawson, P., Martini, M., Scarpa, R., De Luca, G., Milana, G. and Cattaneo, M.: Broadband measurements of sources of explosions at Stromboli volcano, Italy. Geophys. Res. Lett., 26(13), 1937&amp;ndash;1940, 1999. </reference>
		<reference numeration="9" content_type="text">Donoho, D.: On minimum entropy deconvolution, Applied time-series analysis II, Academic Press, 565&amp;ndash;609, 1981. </reference>
		<reference numeration="10" content_type="text">Endo, E.T . and Murray, T.: Real-time seismic amplitude measurement (RSAM): a volcano monitoring and prediction tool, Bull. Volcanol., 53, 533&amp;ndash;545, 1991. </reference>
		<reference numeration="11" content_type="text">Fukao, Y. and Suda, N.: Core modes of the Earth&apos;s free oscillations and structure of the inner core, Geophys. Res. Lett., 16, 401&amp;ndash;404, 1989. </reference>
		<reference numeration="12" content_type="text">Hori, S., Fukao, Y., Kumazawa, M., Furumoto, M. and Yamamoto, A.: A new method of spectral analysis and its application to the Earth&apos;s free oscillations: The &quot;Sompi&quot; method, J. Geophys. Res., 94(B6), 7535&amp;ndash;7553, 1989. </reference>
		<reference numeration="13" content_type="text">Jaquet, O. and Carniel, R.: Stochastic modelling at Stromboli: a volcano with remarkable memory. J. Volcanol. Geotherm. Res., 105, 249&amp;ndash;262, 2001. </reference>
		<reference numeration="14" content_type="text">Jousset, P., Neuberg, J., and Sturton, S.: Modelling the time-frequency content of low-frequency volcanic earthquakes, J. Volcanol. Geotherm. Res., 128, 201&amp;ndash;223, 2003. </reference>
		<reference numeration="15" content_type="text">Kay, S. M.: Modern spectral estimation, theory and application, Academic Press, 1981. </reference>
		<reference numeration="16" content_type="text">Kumagai, H. and Chouet, B. A.: Acoustic properties of a crack containing magmatic or hydrothermal fluids, J. Geophys; Res., 105(B11), 25 493&amp;ndash;25 512, 2000. </reference>
		<reference numeration="17" content_type="text">Kumagai, H., Chouet, B. A., and Nakano, M.: Temporal evolution of a hydrothermal system in Kusatsu-Shirane Volcano, Japan, inferred from complex frequencies of long-period events, J. Geophys. Res., 107(B10), 2236, doi:10.1029/2001JB000653, 2002. </reference>
		<reference numeration="18" content_type="text">Kumazawa, M., Imanishi, Y., Fukao, Y., Furumoto, M., and Yamamoto, A. A.: Theory of spectral analysis based on the characteristic property of a linear system, Geophys. J. Int., 101, 613&amp;ndash;630, 1990. </reference>
		<reference numeration="19" content_type="text">Lacoume, J.-L., Amblard, P.-O., and Comon, P.: Statistiques d&apos;ordre supérieur pour le traitement du signal, Masson, Paris, 1997. </reference>
		<reference numeration="20" content_type="text">Lesage, P. and Surono: Seismic precursors of the 10~February~1990 eruption of Kelut volcano, Java. J. Volcanol. Geotherm. Res., 65, 135&amp;ndash;146, 1995. </reference>
		<reference numeration="21" content_type="text">Lesage, P., Glangeaud, F. and Mars, J.: Applications of autoregressive and time-frequency analysis to the study of volcanic tremor and LP events, J. Volcanol. Geotherm. Res., 114, 391&amp;ndash;417, 2002. </reference>
		<reference numeration="22" content_type="text">Lesage, P., Mora, M., Alvarado, G., Pacheco, J. F., and Métaxian, J.-P.: Complex behavior and source model of the volcanic tremor at Arenal volcano, Costa Rica, J. Volcanol. Geotherm. Res., 157, 49&amp;ndash;59, 2006. </reference>
		<reference numeration="23" content_type="text">Marple, S. L.: Digital spectral analysis with applications, Prentice Hall, Englewood Cliffs, 1987. </reference>
		<reference numeration="24" content_type="text">Mars, J., Lacoume, J.-L., Mari, J.-L., and Glangeaud, F.: Traitement du signal pour géologues et géophysiciens &amp;ndash; Vol 3, Techniques avancées, Technip, 2004. </reference>
		<reference numeration="25" content_type="text">McNutt, S.: Observations and analysis of B-type earthquakes, explosions, and volcanic tremor at Pavlof volcano, Alaska. Bull. Seis. Soc. Am., 76, 153&amp;ndash;175, 1986. </reference>
		<reference numeration="26" content_type="text">McNutt, S. R.: Seismic monitoring and eruption forecasting of volcanoes: A review of the State-of-the-Art and case histories, in: Monitoring and mitigation of volcano hazards, edited by: R. Scarpa and R.I. Tilling, Springer-Verlag, Berlin, 99&amp;ndash;146, 1996. </reference>
		<reference numeration="27" content_type="text">Nakano, M., Kumagai, H., Kumazawa, M., Yamaoka, K., and Chouet, B.: The excitation and characteristic frequency of the long-period volcanic event: an approach based on an inhomogeneous autoregressive model of a linear dynamic system, J. Geophys. Res., 103, 10 031&amp;ndash;10 046, 1998. </reference>
		<reference numeration="28" content_type="text">Nakano, M., Kumagai, H., and Chouet, B.: Source mechanism of long-period events at Kusatsu-Shirane volcano, Japan, inferred from waveform inversion of the effective excitation functions, J. Volcanol. Geotherm. Res., 122, 139&amp;ndash;164, 2003. </reference>
		<reference numeration="29" content_type="text">Ohminato, T., Chouet, B. A., Dawson, P., and Kedar, S.: Waveform inversion of very long period impulsive signals associated with magmatic injection beneath Kilauea volcano, Hawaii, J. Geophys. Res., 103(B10), 23 839&amp;ndash;23 862, 1998. </reference>
		<reference numeration="30" content_type="text">Richard, G. and Lesage, P.: Autoregressive models of resonators for volcanic tremors using Kurtosis, Phys. Signal Image Processing, Marseille, France, 2001. </reference>
		<reference numeration="31" content_type="text">Schlindwein, V., Wassermann, J., and Scherbaum, F.: Spectral analysis of harmonic tremor signals at Mt Semeru volcano, Indonesia, Geophys. Res. Lett., 22, 1685&amp;ndash;1688, 1995. </reference>
		<reference numeration="32" content_type="text">Seidl, D., Kirbani, S. B., and Brüstle, W.: Maximum entropy spectral analysis of volcanic tremor using data from Etna (Sicily) and Merapi (central Java), Bull. Volcanol., 52, 460&amp;ndash;474, 1990. </reference>
		<reference numeration="33" content_type="text">Sturton, S. and Neuberg, J.: The effects of conduit length and acoustic velocity on conduit resonance: implications for low-frequency events, J. Volcanol. Geotherm. Res., 128, 187&amp;ndash;199, 2006. </reference>
		<reference numeration="34" content_type="text">Vandemeulebrouck, J., Sabroux, J.-C., Halbwachs, M., Surono, Poussielgue, N., Grangeon, J., and Tabbagh, J.: Hydroacoustic noise precursors of the 1990 eruption of Kelut volcano, Indonesia, J. Volcanol. Geotherm. Res., 97, 443&amp;ndash;456, 2000. </reference>
		<reference numeration="35" content_type="text">Vila, J., Macia, R., Kumar, D., Ortiz, R., Moreno, H., and Correig, A. M.: Analysis of the unrest of active volcanoes using variations of the base level noise seismic spectrum, J. Volcanol. Geotherm. Res., 153(1&amp;ndash;2), 11&amp;ndash;20, 2006. </reference>
	</references>
</article>

