Spatiotemporal parameters of anomalous reflections from the ionosphere


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

Analysis of vertical sounding data obtained on the network of domestic stations equipped with Parus-A ionosondes has shown that anomalous reflections from the ionosphere previously detected in Moscow are observed throughout the whole mid-latitude region. It is shown that the longitudinal effect impacts the probability of the appearance of anomalous reflections. Their spatiotemporal scales are determined. The horizontal dimensions of the anomalies, as a rule, range from several tens to several hundred, possibly a thousand, kilometers. The region of altitudes at which anomalous reflections are observed extends from the E region to F2 layer. The frequency range in which they are most often recorded is from 2 to 14 MHz. The time of their existence ranges from a fraction of minutes to many hours.

作者简介

G. Givishvili

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

编辑信件的主要联系方式.
Email: givi@izmiran.ru
俄罗斯联邦, Troitsk, 143190

L. Leshchenko

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

Email: givi@izmiran.ru
俄罗斯联邦, Troitsk, 143190

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2017