Ionospheric D-region Cooling in Response to Variations in Tropospheric Conductivity
A new mechanism for electromagnetic coupling between the electrically active mesosphere and the troposphere is discussed. This effect causes a rapid cooling of the ionospheric D-region electrons under large disturbances in tropospheric conductivity. Consequently, the ionospheric plasma transits to t...
Збережено в:
| Дата: | 2013 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Видавничий дім «Академперіодика»
2013
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| Онлайн доступ: | http://rpra-journal.org.ua/index.php/ra/article/view/749 |
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| Назва журналу: | Radio physics and radio astronomy |
Репозитарії
Radio physics and radio astronomy| Резюме: | A new mechanism for electromagnetic coupling between the electrically active mesosphere and the troposphere is discussed. This effect causes a rapid cooling of the ionospheric D-region electrons under large disturbances in tropospheric conductivity. Consequently, the ionospheric plasma transits to the isothermal state from the nonisothermal state conditioned by large mesospheric electric fields. A simplified electric circuit is suggested for troposphere-mesosphere coupling. |
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