Modelling Paroxysmal and Mild-Strombolian Eruptive Plumes at Stromboli and Mt. Etna on 28 August 2019

Author:

Castorina Giuseppe12ORCID,Semprebello Agostino34ORCID,Gattuso Alessandro3ORCID,Salerno Giuseppe5ORCID,Sellitto Pasquale56ORCID,Italiano Francesco7ORCID,Rizza Umberto8ORCID

Affiliation:

1. Italian Institute for Environmental Protection and Research (ISPRA)—Geological Survey of Italy Department, Via Brancati 48, 00144 Roma, Italy

2. Associazione Meteo Professionisti (AMPRO), Via Francesco Morandini, 00142 Roma, Italy

3. Istituto Nazionale di Geofisica e Vulcanologia (INGV)—Sezione di Palermo, Sede Operativa di Milazzo, Via dei Mille, 98057 Milazzo, Italy

4. Dipartimento di Scienze Matematiche e Informatiche, Scienze Fisiche e Scienze della Terra (MIFT), Università degli Studi di Messina, Viale F. Stagno D’Alcontres, 98166 Messina, Italy

5. Istituto Nazionale di Geofisica e Vulcanologia (INGV)—Osservatorio Etneo, Sezione di Catania, Piazza Roma, 95125 Catania, Italy

6. Univ. Paris Est Créteil and Université de Paris, CNRS, Laboratoire Interuniversitaire des Systèmes Atmosphériques, Institut Pierre Simon Laplace, 94010 Créteil, France

7. National Institute of Oceanography and Applied Geophysics–(OGS)—Geophysics Department, 34010 Sgonico, Italy

8. Institute of Atmospheric Sciences and Climate (ISAC), Unit of Lecce, National Research Council (CNR), 73100 Lecce, Italy

Abstract

Volcanic eruptions pose a major natural hazard influencing the environment, climate and human beings at different temporal and spatial scales. Nevertheless, several volcanoes worldwide are poorly monitored and assessing the impact of their eruptions remains, in some cases, challenging. Nowadays, different numerical dispersion models are largely employed in order to evaluate the potential effects of volcanic plume dispersion due to the transport of ash and gases. On 28 August 2019, both Mt. Etna and Stromboli had eruptive activity; Mt. Etna was characterised by mild-Strombolian activity at summit craters, while at Stromboli volcano, a paroxysmal event occurred, which interrupted the ordinary typical-steady Strombolian activity. Here, we explore the spatial dispersion of volcanic sulphur dioxide (SO2) gas plumes in the atmosphere, at both volcanoes, using the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) considering the ground-measured SO2 amounts and the plume-height as time-variable eruptive source parameters. The performance of WRF-Chem was assessed by cross-correlating the simulated SO2 dispersion maps with data retrieved by TROPOMI and OMI sensors. The results show a feasible agreement between the modelled dispersion maps and TROPOMI satellite for both volcanoes, with spatial pattern retrievals and a total mass of dispersed SO2 of the same order of magnitude. Predicted total SO2 mass for Stromboli might be underestimated due to the inhibition from ground to resolve the sin-eruptive SO2 emission due to the extreme ash-rich volcanic plume released during the paroxysm. This study demonstrates the feasibility of a WRF-Chem model with time-variable ESPs in simultaneously reproducing two eruptive plumes with different SO2 emission and their dispersion into the atmosphere. The operational implementation of this method could represent effective support for the assessment of local-to-regional air quality and flight security and, in case of particularly intense events, also on a global scale.

Funder

IMPACT

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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