Journal
REMOTE SENSING
Volume 13, Issue 11, Pages -Publisher
MDPI
DOI: 10.3390/rs13112225
Keywords
satellite remote sensing; volcanic monitoring; SO2 mass and flux retrievals; Etna eruption
Categories
Funding
- ESA project VISTA [4000128399/19/I-DT]
- INGV project Pianeta Dinamico from MIUR (Fondo finalizzato al rilancio degli investimenti delle amministrazioni centrali dello Stato e allo sviluppo del Paese) [CUP D53J19000170001, 145/2018, V3-2021]
- INGV Department strategic project 2019 IMPACT
- Belgian F.R.S-FNRS
- ESA S5P MPC [4000117151/16/I-LG]
- Belgium Prodex TRACE-S5P [PEA 4000105598]
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The presence of volcanic clouds in the atmosphere affects various aspects such as air quality, environment, climate, human health, and aviation safety. Satellite measurements have become an essential tool for volcanic monitoring, enabling a cross-comparison of different sensor data to enhance understanding of volcanic activity. The study highlights the importance of considering factors such as eruption characteristics and instrumental sensitivity when analyzing SO2 flux retrievals from satellite data.
The presence of volcanic clouds in the atmosphere affects air quality, the environment, climate, human health and aviation safety. The importance of the detection and retrieval of volcanic SO2 lies with risk mitigation as well as with the possibility of providing insights into the mechanisms that cause eruptions. Due to their intrinsic characteristics, satellite measurements have become an essential tool for volcanic monitoring. In recent years, several sensors, with different spectral, spatial and temporal resolutions, have been launched into orbit, significantly increasing the effectiveness of the estimation of the various parameters related to the state of volcanic activity. In this work, the SO2 total masses and fluxes were obtained from several satellite sounders-the geostationary (GEO) MSG-SEVIRI and the polar (LEO) Aqua/Terra-MODIS, NPP/NOAA20-VIIRS, Sentinel5p-TROPOMI, MetopA/MetopB-IASI and Aqua-AIRS-and compared to one another. As a test case, the Christmas 2018 Etna eruption was considered. The characteristics of the eruption (tropospheric with low ash content), the large amount of (simultaneously) available data and the different instrument types and SO2 columnar abundance retrieval strategies make this cross-comparison particularly relevant. Results show the higher sensitivity of TROPOMI and IASI and a general good agreement between the SO2 total masses and fluxes obtained from all the satellite instruments. The differences found are either related to inherent instrumental sensitivity or the assumed and/or calculated SO2 cloud height considered as input for the satellite retrievals. Results indicate also that, despite their low revisit time, the LEO sensors are able to provide information on SO2 flux over large time intervals. Finally, a complete error assessment on SO2 flux retrievals using SEVIRI data was realized by considering uncertainties in wind speed and SO2 abundance.
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