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Disturbance Effects in the Lowest Ionosphere

1965
Storm effects in the lowest ionosphere depend on production of anomalous ionization in and below the D-layer. This ionization can be studied by measuring its absorbing effect on radio waves and also by observing some other influences on propagation of VLF and LF radio waves, which are normally reflected at D-layer heights.
openaire   +1 more source

Ionospheric and magnetospheric anomalies and disturbances

Planetary and Space Science, 1964
Abstract Gross deviations from Chapman's well-known theory of F-layer formation are referred to as anomalies (always present) and disturbances (occurring during geomagnetically disturbed periods). In spite of the success of Martyn's drift theory some anomalies and disturbances remain unexplained.
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New Type of Ionospheric Disturbance

Nature, 1970
REGULAR ionospheric soundings close to the magnetic equator in India were started in October 1964 with the installation of a C4 ionosonde at Thumba (magnetic latitude 0.3° S). Soundings were made once every hour during the first 2 years, but have been more frequent, and once every 15 min since January 1967.
openaire   +1 more source

Global Propagation of Ionospheric Disturbances Associated With the 2022 Tonga Volcanic Eruption

Geophysical Research Letters, 2022
Anthony McCaffrey   +2 more
exaly  

Identification of Large-Scale Travelling Ionospheric Disturbances (LSTIDs) Based on Digisonde Observations

Atmosphere, 2023
Konstantinos Tziotziou   +2 more
exaly  

2022 Tonga Volcanic Eruption Induced Global Propagation of Ionospheric Disturbances via Lamb Waves

Frontiers in Astronomy and Space Sciences, 2022
Juha Vierinen   +2 more
exaly  

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