This paper analyzes the mean daily variations of the Earth’s magnetic field recorded at the Yangibazar Geophysical Research Observatory during periods of strong magnetic storms (Kp ≥ 7, Dst ≤ −100 nT). The study examines the diurnal dynamics, amplitude variations, and phase shifts of the main magnetic field components—H, D, and Z. The obtained results show that during strong magnetic storms, daily magnetic variations significantly increase compared to background levels and undergo notable structural changes. The findings are of great importance for the assessment and possible forecasting of earthquakes, as well as for improving regional geophysical monitoring systems.
| Mualliflar | Egamberdiyev, Saidigani, Khusomiddinov, Ahror, Ruzimboev, Farrukh, Jurayev, Elyor, Эгамбердиев, Сайдигани, Хусомиддинов, Ахрор, Рузимбоев, Фаррух, Жураев, Элёр, Egamberdiyev, Saidigani, Husomiddinov, Ahror, Ruzimboev, Farrux, Jo‘rayev, Elyor |
|---|---|
| Jurnal | Саноатда рақамли технологиялар |
| Nashr sanasi | 2026-04-05 |
| Jild | 4 |
| Son | 1 |
| Betlar | 159-165 |
| Til | Rus |
| DOI | 10.70769/3030-3214.srt.4.1.2026.39 |
DOI: 10.70769/3030-3214.srt.4.1.2026.39 · Maqolaning asl sahifasi
strong magnetic storms, Earth’s magnetic field, Yangibazar Observatory, daily variations, geomagnetic activity, сильные магнитные бури, магнитное поле Земли\, суточные вариации, геомагнитная активность\, Янгибазарская, kuchli magnit bo‘ronlari, Yer magnit maydoni, sutkalik variatsiyalar, geomagnit faollik, Yangibazar observatoriyasi
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