VLF phase and amplitude: daytime ionospheric parameters
By Wayne M. McRae, N. Thomson. 2000
159 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/d0fda918b4fbe7692d44ad4c4545d9e981ed5ffd
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Citations in the corpus
- Solar flare induced ionospheric D-region enhancements from VLF amplitude observations (2001, methodology): “These variations have been reported on in more detail by Thomson (1993) and McRae and Thomson (2000). A small solar 'are gives rise to only a small VLF amplitude change accompanying the small perturbation in the D-region ionisation; the resulting peak VLF amplitude clearly depends not only on the si”
- Large solar flares and their ionospheric D region enhancements (2005, background): “affect VLF phase and this occurs progressively with changing daytime solar zenith angle; it is not simply a matter of being either day or night [ McRae and Thomson, 2000, 2004 ].”
- Long‐range lightning geolocation using a VLF radio atmospheric waveform bank (2010, background): “1, for an increase in ionospheric height from 70 km for daytime [McRae and Thomson, 2000] to 85 km for nighttime [Thomson et al.”