Features of Winter Thunderstorms in Kamchatka


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

Winter thunderstorms in Kamchatka are a rare meteorological phenomenon. Temporal variations of the quasi-static electric field and meteorological values at the Paratunka observatory of the Institute of Cosmophysical Research and Radio Wave Propagation, Far East Branch, Russian Academy of Sciences (φ = 52.97° N; λ = 158.25° E), as well as data on solar, seismic and cyclonic activities available on INTERNET, are used to study the nature of this phenomenon. It is shown that powerful solar flares accompanied by increased radiation in the visible and infrared spectra, as well as the infrared radiation from the Earth that enters the atmosphere before powerful earthquakes with a magnitude of M > 8 may serve as an additional heat source in the surface atmosphere of Kamchatkan for the formation of thunderstorm activity. The contribution of tropical cyclones to these processes with weak seismic activity is not clearly defined and requires further detailed study.

Авторлар туралы

S. Smirnov

Institute of Cosmophysical Research and Radio Wave Propagation, Far East Branch, Russia Academy of Sciences

Хат алмасуға жауапты Автор.
Email: sergey@ikir.ru
Ресей, Paratunka, Kamchatka krai, 684034

Yu. Mikhailov

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation

Хат алмасуға жауапты Автор.
Email: yumikh@izmiran.ru
Ресей, TroitskMoscow, 108840

G. Mikhailova

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation

Email: yumikh@izmiran.ru
Ресей, TroitskMoscow, 108840

O. Kapustina

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation

Email: yumikh@izmiran.ru
Ресей, TroitskMoscow, 108840

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