Tropospheric and Ionospheric Anomalies Induced by Volcanic and Saharan Dust Events as Part of Geosphere Interaction Phenomena

Authors

Valerio Tramutoli, University of BasilicataFollow
Francesco Marchese, Italian Research Council
Alfredo Falconieri, Italian Research CouncilFollow
Carolina Filizzola, Italian Research CouncilFollow
Nicola Genzano, University of BasilicataFollow
Katsumi Hattori, Chiba UniversityFollow
Mariano Lisi, University of BasilicataFollow
Jann-Yenq Liu, National Central UniversityFollow
Dimitar Ouzounov, Chapman UniversityFollow
Michel Parrot, Centre National de la Recherche ScientifiqueFollow
Nicola Pergola, Italian Research CouncilFollow
Sergey Pulinets, Russian Academy of SciencesFollow

Document Type

Article

Publication Date

4-17-2019

Abstract

In this work, we assessed the possible relation of ionospheric perturbations observed by Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions (DEMETER), Global Positioning System total electron content (GPS TEC), National Oceanic and Atmospheric Administration (NOAA)-derived outgoing longwave-Earth radiation (OLR), and atmospheric chemical potential (ACP) measurements, with volcanic and Saharan dust events identified by ground and satellite-based medium infrared/thermal infrared (MIR/TIR) observations. The results indicated that the Mt. Etna (Italy) volcanic activity of 2006 was probably responsible for the ionospheric perturbations revealed by DEMETER on 4 November and 6 December and by GPS TEC observations on 4 November and 12 December. This activity also aected the OLR (on 26 October; 6 and 23 November; and 2, 6, and 14 December) and ACP (on 31 October–1 November) analyses. Similarly, two massive Saharan dust episodes, detected by Robust Satellite Techniques (RST) using Spinning Enhanced Visible and Infrared Imager (SEVIRI) optical data, probably caused the ionospheric anomalies recorded, based on DEMETER and GPS TEC observations, over the Mediterranean basin in May 2008. The study confirmed the perturbing eects of volcanic and dust events on tropospheric and ionospheric parameters. Further, it demonstrated the advantages of using independent satellite observations to investigate atmospheric phenomena, which may not always be well documented. The impact of this increased detection capacity in reducing false positives, in the framework of a short-term seismic hazard forecast based on the study of ionospheric and tropospheric anomalies, is also addressed.

Comments

This article was originally published in Geosciences, volume 9, in 2019. DOI: 10.3390/geosciences9040177

Recommended Citation

Tramutoli, V.; Marchese, F.; Falconieri, A.; Filizzola, C.; Genzano, N.; Hattori, K.; Lisi, M.; Liu, J-Y.; Ouzounov, D.; Parrot, M.; Pergola, N.; Pulinets, S. Tropospheric and ionospheric anomalies induced by volcanic and Saharan dust events as part of geosphere interaction phenomena. Geosciences 2019, 9, 177; doi:10.3390/geosciences9040177

Peer Reviewed

1

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Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 License.