Ionospheric and Meteorological Anomalies Associated with the Earthquake in Central Asia on 22 January 2024

On 22 January 2024, at 18 UT, a strong earthquake (EQ), Mw = 7, occurred with the epicenter at 41°N, 79°E. This seismic event generated a complex response, the elements of which correspond to the concept of lithosphere–atmosphere–ionosphere coupling through electromagnetic processes. While flying over the EQ area on the night-ide of the Earth, the tandem of low-orbiting Swarm satellites observed small-scale irregularities in the plasma density with an amplitude of ~1.5 × 104 el/cm3, which are likely associated with the penetration of the coseismic electric field into the ionosphere. The local anomaly was detected against the background of a global increase in total electron content, TEC (although geomagnetic indices remained quiet), since the moment of EQ coincided with the ionospheric response to a solar flare. In the troposphere, specific humidity decreased while latent heat flux and aerosol optical depth increased, all exhibiting the co-located disturbances that can be attributed to the effect of increased air ionization rates, resulting in greater electrical conductivity in the near-Earth boundary layer. Anomalies started developing over the epicenter the day before and maximized on the day of the main shock and aftershocks.

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Publication Details

Journal
Remote Sensing
Published
2024-08-23
DOI
https://doi.org/10.3390/rs16173112
Citations
8
Primary Topic
Earthquake Detection and Analysis
Type
article
Field-Weighted Citation Impact
4.28
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article

Ionospheric and Meteorological Anomalies Associated with the Earthquake in Central Asia on 22 January 2024

Akgenzhe Siylkanova, Renata Lukianova, Gulbanu Daurbayeva
8 citations
Remote Sensing
Earthquake Detection and Analysis
4.28
article

Ionospheric and Meteorological Anomalies Associated with the Earthquake in Central Asia on 22 January 2024

Akgenzhe Siylkanova, Renata Lukianova, Gulbanu Daurbayeva
article en
8 citations

Abstract

On 22 January 2024, at 18 UT, a strong earthquake (EQ), Mw = 7, occurred with the epicenter at 41°N, 79°E. This seismic event generated a complex response, the elements of which correspond to the concept of lithosphere–atmosphere–ionosphere coupling through electromagnetic processes. While flying over the EQ area on the night-ide of the Earth, the tandem of low-orbiting Swarm satellites observed small-scale irregularities in the plasma density with an amplitude of ~1.5 × 104 el/cm3, which are likely associated with the penetration of the coseismic electric field into the ionosphere. The local anomaly was detected against the background of a global increase in total electron content, TEC (although geomagnetic indices remained quiet), since the moment of EQ coincided with the ionospheric response to a solar flare. In the troposphere, specific humidity decreased while latent heat flux and aerosol optical depth increased, all exhibiting the co-located disturbances that can be attributed to the effect of increased air ionization rates, resulting in greater electrical conductivity in the near-Earth boundary layer. Anomalies started developing over the epicenter the day before and maximized on the day of the main shock and aftershocks.

Remote SensingVol. 16(17)
Space Research Institute (RU), National Center of Space Research and Technology (KZ)
Openalex Percentile: Top 5%
Earthquake Detection and Analysis
4.28
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