Abstract

More than 1500 volcanoes can potentially enter into eruption but only some tens of them are equipped with monitoring networks. Most of volcanic eruptions can be predicted by the integration of continuous real time observations, data processing and analysing. In the electromagnetic field (EM), a long history of ground observations shows that electric, magnetic and electromagnetic signals may precede and accompany volcanic eruptions. The possibility that volcanic eruptions may also be preceded by transient electromagnetic anomalies in the ionosphere can be analysed on the basis of DEMETER mission. This microsatellite, launched by CNES in 2004, covers 14 orbits per day over seismic and volcanic regions of the Earth. Two complementary and systematic studies are presented. Over the time period 2004 August–2007 December, the first study shows that three types of electric and/or magnetic anomalies can be observed in the time window of 30 d preceding an eruption and 15 d after. On the 74 eruptions occurring on 50 volcanoes under consideration, 48 anomalies are recognised along 30 eruptions. 41 per cent of the eruptions were accompanied by EM signals on board of the satellite. 81 per cent of the anomalies are observed before the eruptions for the period (−30 d, +15 d) and 69 per cent for the period (−15 d, +15 d). In the second study, the anomalies above three nearby volcanoes (Lopevi, Ambrym and Aoba) are systematically looked for all orbits between 2004 August and 2006 December. Anomalies are only observed during periods of larger activity on each of them. Taking into account that no anomaly is observed a long time before an eruption, on can allocate the anomalies to each volcano. Although the database is still limited, the study shows that volcanic activity may be preceded by EM perturbations of the ionosphere.

Highlights

  • Only some tens of volcanoes in the world are monitored by complex geophysical equipments, whereas hundreds of volcanoes remain without any adequate observations and real time monitoring systems

  • Microsatellite DEMETER, launched in 2004 June by the French National Space Agency (CNES), is devoted to the detection of electromagnetic (EM) perturbations of the ionosphere caused by earthquakes, volcanic eruptions and human activities (Berthelier et al 2006; Colin et al 2006; Lebreton et al 2006; Parrot et al 2006a; Sauvaud et al 2006; Zlotnicki et al 2006)

  • To study the disturbances of the ionosphere generated by seismoand volcano-electromagnetic effects, and anthropogenic activities, a specific instrumentation is operating for measuring the electromagnetic field and the plasma characteristics

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Summary

INTRODUCTION

Number of studies stand on the possibility to identify precursory signals to natural disasters as volcanic eruptions and earthquakes. Yukutake et al 1990a, 1990b; Hashimoto & Tanaka 1995; Tanaka 1995; Zlotnicki et al 2000, 2001, 2006; Sasai et al 2001, 2002; Del Negro & Currenti 2003; Del Negro et al 2004) Mechanisms of these electric and magnetic signals can be found in review papers (i.e. Johnston 1997; Zlotnicki & Nishida 2003). The. C 2010 The Authors Geophysical Journal International C 2010 RAS microsatellite DEMETER, launched in 2004 June by the French National Space Agency (CNES), is devoted to the detection of electromagnetic (EM) perturbations of the ionosphere caused by earthquakes, volcanic eruptions and human activities (Berthelier et al 2006; Colin et al 2006; Lebreton et al 2006; Parrot et al 2006a; Sauvaud et al 2006; Zlotnicki et al 2006). This paper is an attempt to recognize EM signals related to volcanic activity in the data recorded on DEMETER satellite

DEMETER MISSION AND DATABASE
DEMETER instrumentation
Database
Method
Type 1
Type 2
Type 3
Analysis
Anomalies
Volcanic activity
Discussion
Findings
CONCLUSION
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