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Giuseppe Giovanni Salerno, BSc

PhD student

Volcanic degassing at Mt. Etna and Stromboli (Italy): high time resolution measurements and models

Biography

Following his first degree in Earth Sciences, Giuseppe qualified as a Chartered Geologist and then completed a certificate course in Remote Sensing and GIS at the University of Naples. In 2001, he took a research position with the Istituto Nazionale di Geofisica e Vulcanologia (INGV) in Catania (Italy), joining the Geochemistry Remote Sensing Group. From 2002 to 2004 he was supported by scholarships from the Italian Space Agency (ASI) and INGV, as part of the FASA European Project. In 2002 he followed a graduate course in Volcanology at the University of Catania and, in 2005, the International Training Program in volcanology on Hawai'i with CSAV (University of Hawai'i - Hilo) and USGS (United States Geological Survey).

Giuseppe's doctoral research focuses on: (i) differential optical absorption spectroscopy (DOAS) of SO2 emissions from Stromboli and Etna using ultraviolet remote sensing methods; (ii) interpretation of magma dynamics from integrated geochemical and geophysical observations; (iii) development and installation of new remote sensing tools for monitoring of active volcanoes.

Since 2001, when he joined INGV, he has been very closely involved in the monitoring and emergency response to volcaninc crisis of Mt. Etna and the 2002 eruption of Stromboli.

Career

Qualifications

Research

Supervisors: Clive Oppenheimer and Dr. Mike Burton of Istituto Nazionale di Geofisica e Vulcanologia, Catania, (Italy).

Observations of volcanic gas emissions are essential to improving our understanding of magma dynamics and the style of eruptions. Active volcanoes are a major source for many gas species, and their emissions play important roles in atmospheric and climatic processes, and can also adversely impact public health in downwind communities. For example, approximately 10% of the global flux of SO2 injected into the atmosphere has been attributed to volcanic activity [Bluth et al. 1993]. Sulphur dioxide is one of the three most abundant magmatic gases (after H2O and CO2). SO2 fluxes are directly linked to magma supply rates because this gas species is exsolved during the decompression of magma upon ascent. Knowledge of the sulphur content of undegassed magma and the final sulphur concentration in erupted products permits estimates of magma supply rates from observed SO2 emission rates (Allard et al., Nature; Francis et al., Nature).

Measurement of SO2 fluxes from volcanoes has been carried out using ultraviolet remote sensing techniques for over 30 years and has become a standard practice in volcano surveillance. Recent technological advances have led to the availability of lightweight UV spectrometers suitable for measuring SO2 emissions from volcanoes [e.g. Galle et al, 2003; McGonigle et al, 2004]. The availability of these instruments provides the opportunity for intensive measurements of SO2 fluxes at high temporal resolution using fixed arrays of scanning spectrometers [Edmonds et al. 2003]. In 2004 the Istituto Nazionale di Geofisica e Vulcanologia (INGV) Section based in Catania (Italy) designed, built and installed a network of UV scanners on Stromboli (Aeolian Islands) and Mt Etna in order to perform real-time, high temporal resolution measurements of SO2 flux. Two anemometers were installed near the summit of both volcanoes in order to provide wind speed data for the SO2 flux calculations. These high temporal resolution geochemical data represent an important step forward in volcanic surveillance providing real-time information with a time step approaching that of other geophysical datastreams. Furthermore, real-time, daylight volcanic plume scanning provides a method for assessment of volcanic ash-cloud hazard, critical for aviation safety. The key aim of my project is to analyse two-years of SO2 flux data from the new UV scanning arrays on Mt Etna and on Stromboli. This study will enable a critical evaluation of the errors and limits of the detection system, and will provide the basis to determine short-term and long-term variations in magma supply rates at both volcanoes and the relationships between SO2 flux, geophysical parameters, and eruptive style.

Publications

Publications submitted/review

Publications in preparation

External activities

Project and external activities: