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  5. A cross-comparison of thermal infrared versus ultraviolet ground-based retrievals of SO2 masses during Strombolian explosions
 
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A cross-comparison of thermal infrared versus ultraviolet ground-based retrievals of SO2 masses during Strombolian explosions

Journal
VOLCANICA
ISSN
2610-3540
Date Issued
2025-12-15
Author(s)
Del Bello, Elisabetta  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Bagnato, Emanuela  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Guerrieri, Lorenzo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Tamburello, Giancarlo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia  
Corradini, Stefano  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Merucci, Luca  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Pennacchia, Francesco  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Scarlato, Piergiorgio  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Stelitano, Dario  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Taddeucci, Jacopo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
DOI
10.30909/vol/sgic1814
Abstract
This study investigates sulfur dioxide (SO2) emissions from Stromboli’s explosive activity using ground-based remote sensing techniques. We analyze the SO2 mass derived from ultraviolet (UV) and thermal infrared (TIR) cameras, alongside explosion parameters and emitted products obtained from high-frequency thermal imaging. Our dataset (May 23–24, 2023) includes 49 explosions ranging from gas-dominated (Type 0) to bomb-dominated (Type 1) and ash-rich (Type 2). During non-explosive periods, UV and TIR SO2 masses are generally comparable, whereas explosions show systematic TIR overestimation relative to UV. The TIR/UV deviation scales with plume temperature and eruption type, reflecting TIR sensitivity to thermal radiation and ash scattering, while UV retrievals remain largely temperature-independent. Our results emphasize the need for temperature-based corrections in TIR retrievals, and support integrated multi-sensor approaches for robust, real-time monitoring of volcanic gas emissions.
Subjects

Volcanic degassing

Strombolian explosion...

SO 2 mass estimation

UV camera

Thermal infrared imag...

Stromboli

File(s)
Main Article: DellBello_et_al-2025_Volcanica.pdf (3.54 MB)
rome library|catania library|milano library|napoli library|pisa library|palermo library
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