Unoccupied Aircraft Systems (UASs) Reveal the Morphological Changes at Stromboli Volcano (Italy) before, between, and after the 3 July and 28 August 2019 Paroxysmal Eruptions

In July and August 2019, two paroxysmal eruptions dramatically changed the morphology of the crater terrace that hosts the active vents of Stromboli volcano (Italy). Here, we document these morphological changes, by using 2259 UAS-derived photographs from eight surveys and Structure-from-Motion (SfM) photogrammetric techniques, resulting in 3D point clouds, orthomosaics, and digital surface models (DSMs) with resolution ranging from 8.1 to 12.4 cm/pixel. We focus on the morphological evolution of volcanic features and volume changes in the crater terrace and the upper part of the underlying slope (Sciara del Fuoco). We identify both crater terrace and lava field variations, with vents shifting up to 47 m and the accumulation of tephra deposits. The maximum elevation changes related to the two paroxysmal eruptions (in between May and September 2019) range from +41.4 to −26.4 m at the lava field and N crater area, respectively. Throughout September 2018–June 2020, the total volume change in the surveyed area was +447,335 m3. Despite Stromboli being one of the best-studied volcanoes worldwide, the UAS-based photogrammetry products of this study provide unprecedented high spatiotemporal resolution observations of its entire summit area, in a period when volcanic activity made the classic field inspections and helicopter overflights too risky. Routinely applied UAS operations represent an effective and evolving tool for volcanic hazard assessment and to support decision-makers involved in volcanic surveillance and civil protection operations.

[1]  J. Arrowsmith,et al.  The emplacement of the active lava flow at Sinabung Volcano, Sumatra, Indonesia, documented by structure-from-motion photogrammetry , 2019, Journal of Volcanology and Geothermal Research.

[2]  Riccardo Fanti,et al.  Environmental Aftermath of the 2019 Stromboli Eruption , 2020, Remote. Sens..

[3]  M. Pistolesi,et al.  The November 2009 paroxysmal explosions at Stromboli. , 2010 .

[4]  J. Rau,et al.  The use of UAV remote sensing for observing lava dome emplacement and areas of potential lahar hazards: An example from the 2017–2019 eruption crisis at Mount Agung in Bali , 2021, Journal of Volcanology and Geothermal Research.

[5]  T. Caltabiano,et al.  Major eruptive style changes induced by structural modifications of a shallow conduit system: the 2007–2012 Stromboli case , 2014, Bulletin of Volcanology.

[6]  A. Peccerillo,et al.  Chapter 11 Geology, volcanic history and petrology of Vulcano (central Aeolian archipelago) , 2013 .

[7]  M. Ripepe,et al.  Forecasting Effusive Dynamics and Decompression Rates by Magmastatic Model at Open-vent Volcanoes , 2017, Scientific Reports.

[8]  M. Cantarero,et al.  UAVs for volcano monitoring: A new approach applied on an active lava flow on Mt. Etna (Italy), during the 27 February–02 March 2017 eruption , 2019, Journal of Volcanology and Geothermal Research.

[9]  S. Robson,et al.  Straightforward reconstruction of 3D surfaces and topography with a camera: Accuracy and geoscience application , 2012 .

[10]  Nicola Casagli,et al.  Overflows and Pyroclastic Density Currents in March-April 2020 at Stromboli Volcano Detected by Remote Sensing and Seismic Monitoring Data , 2020, Remote. Sens..

[11]  M. Ripepe,et al.  The Stromboli Volcano: An Integrated Study of the 2002–2003 Eruption—Introduction , 2013 .

[12]  A. Graziani,et al.  Modelling the instability phenomena on the NW flank of Stromboli Volcano (Italy) due to lateral dyke intrusion , 2019, Journal of Volcanology and Geothermal Research.

[13]  Nicola Pergola,et al.  The July/August 2019 Lava Flows at the Sciara del Fuoco, Stromboli-Analysis from Multi-Sensor Infrared Satellite Imagery , 2019, Remote. Sens..

[14]  Jeffrey B. Johnson,et al.  UAS-based tracking of the Santiaguito Lava Dome, Guatemala , 2020, Scientific Reports.

[15]  Nicola Casagli,et al.  The 2014 Effusive Eruption at Stromboli: New Insights from In Situ and Remote-Sensing Measurements , 2018, Remote. Sens..

[16]  Benjamin R. Jordan,et al.  Collecting field data in volcanic landscapes using small UAS (sUAS)/drones , 2019, Journal of Volcanology and Geothermal Research.

[17]  Nicola Casagli,et al.  Variable Magnitude and Intensity of Strombolian Explosions: Focus on the Eruptive Processes for a First Classification Scheme for Stromboli Volcano (Italy) , 2021, Remote. Sens..

[18]  G. Giordano,et al.  The summer 2019 basaltic Vulcanian eruptions (paroxysms) of Stromboli , 2020, Bulletin of Volcanology.

[19]  R. Civico,et al.  Characterising vent and crater shape changes at Stromboli: implications for risk areas , 2021, Volcanica.

[20]  L. Francalanci,et al.  Chapter 13 Eruptive, volcano-tectonic and magmatic history of the Stromboli volcano (north-eastern Aeolian archipelago) , 2013 .

[21]  Maria Fabrizia Buongiorno,et al.  Ten years of volcanic activity at Mt Etna: High-resolution mapping and accurate quantification of the morphological changes by Pleiades and Lidar data , 2021, Int. J. Appl. Earth Obs. Geoinformation.

[22]  Mike R. James,et al.  Thermal photogrammetric imaging: A new technique for monitoring dome eruptions , 2017 .

[23]  A. Sonnessa,et al.  Photogrammetric and LIDAR surveys on the Sciara del Fuoco to monitor the 2007 Stromboli eruption , 2008, 2008 Second Workshop on Use of Remote Sensing Techniques for Monitoring Volcanoes and Seismogenic Areas.

[24]  M. Rosi,et al.  Chronology of the 2007 eruption of Stromboli and the activity of the Scientific Synthesis Group , 2009 .

[25]  A. Cannata,et al.  Shallow conduit dynamics fuel the unexpected paroxysms of Stromboli volcano during the summer 2019 , 2021, Scientific Reports.

[26]  A. Favero,et al.  Italy , 1996, The Lancet.

[27]  M. Pistolesi,et al.  Paroxysms at Stromboli Volcano (Italy): Source, Genesis and Dynamics , 2021, Frontiers in Earth Science.

[28]  A. Esposito,et al.  Geophysical precursors of the July-August 2019 paroxysmal eruptive phase and their implications for Stromboli volcano (Italy) monitoring , 2020, Scientific Reports.

[29]  N. Casagli,et al.  Joint exploitation of space-borne and ground-based multitemporal InSAR measurements for volcano monitoring: The Stromboli volcano case study , 2021, Remote Sensing of Environment.

[30]  S. Inguaggiato,et al.  Changes in CO2 Soil Degassing Style as a Possible Precursor to Volcanic Activity: The 2019 Case of Stromboli Paroxysmal Eruptions , 2020, Applied Sciences.

[31]  Thomas R. Walter,et al.  Volcanological applications of unoccupied aircraft systems (UAS): Developments, strategies, and future challenges , 2020 .

[32]  Daniele Andronico,et al.  Characterizing high energy explosive eruptions at Stromboli volcano using multidisciplinary data: An example from the 9 January 2005 explosion , 2008 .

[33]  A. Harris,et al.  Integrating puffing and explosions in a general scheme for Strombolian‐style activity , 2017 .

[34]  M. Neri,et al.  Dyke emplacement and related hazard in volcanoes with sector collapse: the 2007 Stromboli (Italy) eruption , 2008, Journal of the Geological Society.

[35]  A. Tibaldi,et al.  Geological‐Structural Framework of Stromboli Volcano, Past Collapses, and the Possible Influence on the Events of the 2002–2003 Crisis , 2013 .

[36]  Stromboli eruption : event chronology and effusion rates using 1 thermal infrared data 2 3 , 2022 .

[37]  J. Taddeucci,et al.  The 15 March 2007 paroxysm of Stromboli: video-image analysis, and textural and compositional features of the erupted deposit , 2013, Bulletin of Volcanology.

[38]  Daniele Andronico,et al.  Parameterizing multi-vent activity at Stromboli Volcano (Aeolian Islands, Italy) , 2018, Bulletin of Volcanology.

[39]  Paolo Baldi,et al.  The morphological evolution of the Sciara del Fuoco since 1868: reconstructing the effusive activity at Stromboli volcano , 2011, Bulletin of Volcanology.

[40]  J. Taddeucci,et al.  Uncovering the eruptive patterns of the 2019 double paroxysm eruption crisis of Stromboli volcano , 2021, Nature Communications.

[41]  Nicola Casagli,et al.  Catching Geomorphological Response to Volcanic Activity on Steep Slope Volcanoes Using Multi-Platform Remote Sensing , 2020, Remote. Sens..

[42]  Subandriyo,et al.  Morphological and structural changes at the Merapi lava dome monitored in 2012–15 using unmanned aerial vehicles (UAVs) , 2018 .

[43]  M. Pompilio,et al.  Chapter 14 Stromboli volcano, Aeolian Islands (Italy): present eruptive activity and hazards , 2013 .

[44]  H. Gunawan,et al.  Monitoring, forecasting collapse events, and mapping pyroclastic deposits at Sinabung volcano with satellite imagery , 2019, Journal of Volcanology and Geothermal Research.

[45]  A. Harris,et al.  The 2007 Stromboli eruption: event chronology and effusion rates using thermal infrared data , 2010 .

[46]  A. Bertagnini,et al.  Volcanology and Magma Geochemistry of the Present‐Day Activity: Constraints on the Feeding System , 2008 .

[47]  M. Favalli,et al.  The 2004–2005 Mt. Etna Compound Lava Flow Field: A Retrospective Analysis by Combining Remote and Field Methods , 2021, Journal of Geophysical Research: Solid Earth.

[48]  Stuart Robson,et al.  Sequential digital elevation models of active lava flows from ground-based stereo time-lapse imagery , 2014 .

[49]  A. Tibaldi Multiple sector collapses at stromboli volcano, Italy: how they work , 2001 .

[50]  Takayuki Nakano,et al.  LANDFORM MONITORING IN ACTIVE VOLCANO BY UAV AND SFM-MVS TECHNIQUE , 2014 .

[51]  Mona Hess,et al.  Structure from Motion: Photogrammetry , 2017 .

[52]  M. Ripepe,et al.  Radiative heat power at Stromboli volcano during 2000-2011: Twelve years of MODIS observations , 2012 .

[53]  Simone Tarquini,et al.  Evolution of an active lava flow field using a multitemporal LIDAR acquisition , 2010 .

[54]  N. Casagli,et al.  Deformation of Stromboli Volcano (Italy) during the 2007 eruption revealed by radar interferometry, numerical modelling and structural geological field data , 2009 .

[55]  K. Befus,et al.  Rhyolite lava emplacement dynamics inferred from surface morphology , 2020, Journal of Volcanology and Geothermal Research.

[56]  M. James,et al.  Detecting the development of active lava flow fields with a very‐long‐range terrestrial laser scanner and thermal imagery , 2009 .

[57]  Paul J. Besl,et al.  A Method for Registration of 3-D Shapes , 1992, IEEE Trans. Pattern Anal. Mach. Intell..

[58]  J. Taddeucci,et al.  The dynamics of explosive mafic eruptions: New insights from multiparametric observations , 2021 .

[59]  N. Casagli,et al.  From hot rocks to glowing avalanches: Numerical modelling of gravity-induced pyroclastic density currents and hazard maps at the Stromboli volcano (Italy) , 2016 .

[60]  J. Chandler,et al.  A convergent image configuration for DEM extraction that minimises the systematic effects caused by an inaccurate lens model , 2008 .