Global ionospheric radio observatory (GIRO)
BW Reinisch, IA Galkin - Earth, planets and space, 2011 - Springer
Digisonde ionospheric sounders installed at 80+ locations in the world have gradually
evolved their generally independent existence into a Global Ionospheric Radio Observatory …
evolved their generally independent existence into a Global Ionospheric Radio Observatory …
Electric field penetration into Earth's ionosphere: a brief review for 2000–2013
Electric field penetration is a consequence of solar wind interaction with planetary
magnetosphere and/or ionosphere. For both Earth with intrinsic magnetosphere and …
magnetosphere and/or ionosphere. For both Earth with intrinsic magnetosphere and …
Ionospheric F-region response to geomagnetic disturbances
AD Danilov - Advances in Space Research, 2013 - Elsevier
The F2-region reaction to geomagnetic storms usually called as an ionospheric storm is a
rather complicated event. It consists of so called positive and negative phases, which have …
rather complicated event. It consists of so called positive and negative phases, which have …
East–west difference in the ionospheric response during the recovery phase of May 2024 super geomagnetic storm over the East Asian
X Guo, B Zhao, T Yu, H Hao, W Sun… - Journal of …, 2024 - Wiley Online Library
In this study, we offer an extensive examination of the F‐region ionospheric disturbances
during the May 2024 superstorm, focusing primarily on the middle‐low latitude regions of …
during the May 2024 superstorm, focusing primarily on the middle‐low latitude regions of …
Recent results and outstanding questions on the response of the electrodynamics of the low latitude ionosphere to solar wind and magnetospheric disturbances
Storm-time ionospheric electrodynamics effects have been the subject of extensive studies.
The solar wind/magnetosphere/ionosphere and thermosphere disturbance wind dynamos …
The solar wind/magnetosphere/ionosphere and thermosphere disturbance wind dynamos …
A physical mechanism of positive ionospheric storms at low latitudes and midlatitudes
A physical mechanism of the positive ionospheric storms at low latitudes and midlatitudes is
presented through multi‐instrument observations, theoretical modeling, and basic principles …
presented through multi‐instrument observations, theoretical modeling, and basic principles …
Positive and negative ionospheric responses to the March 2015 geomagnetic storm from BDS observations
The most intense geomagnetic storm in solar cycle 24 occurred on March 17, 2015, and the
detailed ionospheric storm morphologies are difficultly obtained from traditional …
detailed ionospheric storm morphologies are difficultly obtained from traditional …
Was magnetic storm the only driver of the long‐duration enhancements of daytime total electron content in the Asian‐Australian sector between 7 and 12 September …
In this study, multiple data sets from Beidou geostationary orbit satellites total electron
contents (TECs), ionosonde, meteor radar, magnetometer, and model simulations have …
contents (TECs), ionosonde, meteor radar, magnetometer, and model simulations have …
Global ionospheric and thermospheric effects of the June 2015 geomagnetic disturbances: Multi‐instrumental observations and modeling
By using data from multiple instruments, we investigate ionospheric/thermospheric behavior
during the period from 21 to 23 June 2015, when three interplanetary shocks (IS) of different …
during the period from 21 to 23 June 2015, when three interplanetary shocks (IS) of different …
Density perturbations in the upper atmosphere caused by the dissipation of solar wind energy
GW Prölss - Surveys in Geophysics, 2011 - Springer
The upper atmosphere constitutes the outer region of the terrestrial gas envelope above
about 100 km altitude. The energy budget of this outer gas layer is partly controlled by the …
about 100 km altitude. The energy budget of this outer gas layer is partly controlled by the …