Модуляция спорадических Е-слоев мелкомасштабными атмосферными волнами в высокоширотной ионосфере Земли

Модуляция спорадических Е-слоев мелкомасштабными атмосферными волнами в высокоширотной ионосфере Земли

Автор: Губенко В.Н., Кириллович И.А.

Журнал: Солнечно-земная физика @solnechno-zemnaya-fizika

Статья в выпуске: 3 т.5, 2019 года.

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Радиозатменные измерения спутника CHAMP (Challenging Minisatellite Payload) были использованы нами для исследования спорадических Е-слоев (высоты 90-130 км) в высокоширотной ионосфере Земли. Разработан новый метод определения характеристик внутренних атмосферных волн, базирующийся на использовании наклонных спорадических Е-слоев ионосферы Земли в качестве детектора. Метод основан на том, что внутренняя волна, распространяющаяся через изначально горизонтальный спорадический E-слой, вызывает вращение градиента плотности плазмы в направлении волнового вектора, что приводит к установлению плоскости слоя параллельно фазовому фронту волны. Разработанный метод позволяет исследовать взаимосвязи между мелкомасштабными внутренними волнами и спорадическими Е-слоями в ионосфере Земли и существенно расширяет возможности традиционного радиозатменного мониторинга атмосферы. Показано, что исследуемые внутренние атмосферные волны имеют периоды от 35 до 46 мин и вертикальные фазовые скорости от 1.2 до 2.0 м/с, что хорошо согласуется с результатами независимых экспериментов и данными моделирования спорадических Е-слоев на высоте ~100 км в полярной шапке Земли.

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Радиозатменные измерения, атмосфера и ионосфера земли, наклонные спорадические е-слои, внутренние атмосферные волны

Короткий адрес: https://sciup.org/142222479

IDR: 142222479   |   DOI: 10.12737/szf-53201912

Список литературы Модуляция спорадических Е-слоев мелкомасштабными атмосферными волнами в высокоширотной ионосфере Земли

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