Thirty years of satellite‐derived lava discharge rates at Etna: Implications for steady volumetric output
Language
English
Obiettivo Specifico
1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
/116 (2011)
Publisher
American Geophysical Union
Pages (printed)
B08204
Date Issued
August 9, 2011
Subjects
Abstract
We present a 30 year long data set of satellite‐derived time‐averaged lava
discharge rates (TADR) for Mount Etna volcano (Sicily, Italy), spanning 1980–2010
and comprising 1792 measurements during 23 eruptions. We use this to classify eruptions
on the basis of magnitude and intensity, as well as the shape of the TADR time series
which characterizes each effusive event. We find that while 1983–1993 was characterized
by less frequent but longer‐duration effusive eruptions at lower TADRs, 2000–2010
was characterized by more frequent eruptions of shorter duration and higher TADRs.
However, roughly the same lava volume was erupted during both of these 11 year long
periods, so that the volumetric output was linear over the entire 30 year period, increasing
at a rate of 0.8 m3 s−1 between 1980 and 2010. The cumulative volume record can be
extended back in time using data available in the literature. This allows us to assess
Etna’s output history over 5 centuries and to place the current trend in historical context.
We find that output has been stable at this rate since 1971. At this time, the output rate
changed from a low discharge rate phase, which had characterized the period 1759 to
1970, to a high discharge rate phase. This new phase had the same output rate as the
high discharge rate phase that characterized the period 1610–1669. The 1610–1669
phase ended with the most voluminous eruption of historic times.
discharge rates (TADR) for Mount Etna volcano (Sicily, Italy), spanning 1980–2010
and comprising 1792 measurements during 23 eruptions. We use this to classify eruptions
on the basis of magnitude and intensity, as well as the shape of the TADR time series
which characterizes each effusive event. We find that while 1983–1993 was characterized
by less frequent but longer‐duration effusive eruptions at lower TADRs, 2000–2010
was characterized by more frequent eruptions of shorter duration and higher TADRs.
However, roughly the same lava volume was erupted during both of these 11 year long
periods, so that the volumetric output was linear over the entire 30 year period, increasing
at a rate of 0.8 m3 s−1 between 1980 and 2010. The cumulative volume record can be
extended back in time using data available in the literature. This allows us to assess
Etna’s output history over 5 centuries and to place the current trend in historical context.
We find that output has been stable at this rate since 1971. At this time, the output rate
changed from a low discharge rate phase, which had characterized the period 1759 to
1970, to a high discharge rate phase. This new phase had the same output rate as the
high discharge rate phase that characterized the period 1610–1669. The 1610–1669
phase ended with the most voluminous eruption of historic times.
Sponsors
This contribution is in support of
the LMV‐based (PI: Franck Donnadieu) TerMex‐MYSTRALS project
“Contribution à l’évaluation des risques associés aux activités éruptives
majeures de l’Etna: approche multidisciplinaire des processus et précurseurs.”
the LMV‐based (PI: Franck Donnadieu) TerMex‐MYSTRALS project
“Contribution à l’évaluation des risques associés aux activités éruptives
majeures de l’Etna: approche multidisciplinaire des processus et précurseurs.”
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Bailey, J. E., A. J. L. Harris, J. Dehn, S. Calvari, and S. K. Rowland (2006),
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(MODIS) on EOS‐AM1, IEEE Trans. Geosci. Remote Sens., 36(4),
1088–1100, doi:10.1109/36.700993.
Behncke, B., and M. Neri (2003a), Cycles and trends in the recent eruptive
behaviour of Mount Etna (Italy), Can. J. Earth Sci., 40, 1405–1411,
doi:10.1139/e03-052.
Behncke, B., and M. Neri (2003b), The July‐August 2001 eruption of
Mt. Etna (Sicily), Bull. Volcanol., 65, 461–476, doi:10.1007/s00445-
003-0274-1.
Behncke, B., M. Neri, E. Pecora, and V. Zanon (2006), The exceptional
activity and growth of the Southeast Crater, Mount Etna (Italy), between
1996 and 2001, Bull. Volcanol., 69, 149–173, doi:10.1007/s00445-006-
0061-x.
Bertagnini, A., N. Métrich, P. Landi, and M. Rosi (2003), Stromboli volcano
(Aeolian Archipelago, Italy): An open window on the deep‐feeding
system of a steady state basaltic volcano, J. Geophys. Res., 108(B7),
2336, doi:10.1029/2002JB002146.
Branca, S., and P. Del Carlo (2004), Eruptions of Mt. Etna during the past
3,200 years: A revised compilation integrating the historical and stratigraphic
records, in Mt. Etna: Volcano Laboratory, Geophys. Monogr.
Ser., vol. 143, edited by A. Bonaccorso et al., pp. 1–27, AGU, Washington,
D. C.
Brown, J. W., O. B. Brown, and R. H. Evans (1993), Calibration of
Advanced Very High Resolution Radiometer infrared channels: A new
approach to nonlinear correction, J. Geophys. Res., 98(C10), 18,257–18,268,
doi:10.1029/93JC01638.
Burton,M., et al. (2005), Etna 2004–05: An archetype for geodynamically controlled
effusive eruptions, Geophys. Res. Lett., 32, L09303, doi:10.1029/
2005GL022527.
Calvari, S., and the Whole Scientific Staff of INGV‐Sezione di Catania
(2001), Multidisciplinary approach yields insight into Mt. Etna 2001
eruption, Eos Trans. AGU, 82(52), 653–656, doi:10.1029/01EO00376.
Calvari, S., M. Coltelli, M. Neri, M. Pompilio, and V. Scribano (1994), The
1991–93 Etna eruption: Chronology and lava flow field evolution, Acta
Vulcanol., 4, 1–14.
Calvari, S., M. Neri, and H. Pinkerton (2003), Effusion rate estimations during
the 1999 summit eruption on Mt. Etna, and growth of two distinct lava
flow fields, J. Volcanol. Geotherm. Res., 119, 107–123, doi:10.1016/
S0377-0273(02)00308-6.
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