Observations of ionospheric disturbances associated with the 2020 Beirut explosion by Defense Meteorological Satellite Program and ground-based ionosondes
-
Published:2024-07-01
Issue:1
Volume:42
Page:301-312
-
ISSN:1432-0576
-
Container-title:Annales Geophysicae
-
language:en
-
Short-container-title:Ann. Geophys.
Author:
Pradipta RezyORCID, Lai Pei-Chen
Abstract
Abstract. A major explosion that released a significant amount of energy into the atmosphere occurred in Beirut on 4 August 2020. The energy released may have reached the upper atmosphere and generated some traveling ionospheric disturbances (TIDs), which can affect radio wave propagation. In this study, we used data from the Defense Meteorological Satellite Program (DMSP) and ground-based ionosondes in the Mediterranean region to investigate the ionospheric response to this historic explosion event. Our DMSP data analysis revealed a noticeable increase in the ionospheric electron density near the Beirut area following the explosion, accompanied by some wavelike disturbances. Some characteristic TID signatures were also identified in the shape of ionogram traces at several locations in the Mediterranean. This event occurred during a period of relatively quiet geomagnetic conditions, making the observed TIDs likely to have originated from the Beirut explosion, not from other sources such as auroral activities. These observational findings demonstrate that TIDs from the Beirut explosion were able to propagate over longer distances, beyond the immediate areas of Lebanon and Israel–Palestine, reaching the Mediterranean and eastern Europe.
Funder
Air Force Office of Scientific Research
Publisher
Copernicus GmbH
Reference61 articles.
1. Belehaki, A., Tsagouri, I., Altadill, D., Blanch, E., Borries, C., Buresova, D., Chum, J., Galkin, I., Juan, J. M., Segarra, A., Camilo Timoté, C., Tziotziou, K., Verhulst, T. G. W., and Watermann, J.: An overview of methodologies for real-time detection, characterisation and tracking of traveling ionospheric disturbances developed in the TechTIDE project, J. Space Weather Space Clim., 10, 42, https://doi.org/10.1051/swsc/2020043, 2020. a 2. Boyde, B., Wood, A., Dorrian, G., Fallows, R. A., Themens, D., Mielich, J., Elvidge, S., Mevius, M., Zucca, P., Dabrowski, B., Krankowski, A., Vocks, C., and Bisi, M.: Lensing from small-scale travelling ionospheric disturbances observed using LOFAR, J. Space Weather Space Clim., 12, 34, https://doi.org/10.1051/swsc/2022030, 2022. a 3. Burke, W. J., Gentile, L. C., Huang, C. Y., Valladares, C. E., and Su, S. Y.: Longitudinal variability of equatorial plasma bubbles observed by DMSP and ROCSAT-1, J. Geophys. Res., 109, A12301, https://doi.org/10.1029/2004JA010583, 2004. a 4. Cervera, M. A. and Harris, T. J.: Modeling ionospheric disturbance features in quasi-vertically incident ionograms using 3-D magnetoionic ray tracing and atmospheric gravity waves, J. Geophys. Res.-Space, 119, 431–440, https://doi.org/10.1002/2013JA019247, 2014. a 5. Cheng, K. and Huang, Y.-N.: Ionospheric disturbances observed during the period of Mount Pinatubo eruptions in June 1991, J. Geophys. Res., 97, 16995–17004, https://doi.org/10.1029/92JA01462, 1992. a
|
|