Ionospheric D Region: Characteristics Near Dawn and Dusk
Thomson, Neil R. ORCID: https://orcid.org/0000-0002-0772-148X; Clilverd, Mark A.
ORCID: https://orcid.org/0000-0002-7388-1529; Rodger, Craig J.
ORCID: https://orcid.org/0000-0002-6770-2707.
2025
Ionospheric D Region: Characteristics Near Dawn and Dusk.
Journal of Geophysical Research: Space Physics, 130 (4), e2024JA033610.
18, pp.
10.1029/2024JA033610
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©2025. The Author(s). JGR Space Physics - 2025 - Thomson - Ionospheric D Region Characteristics Near Dawn and Dusk.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (5MB) | Preview |
Abstract/Summary
The characteristics of very low frequency (VLF) radio wave propagation in the Earth-ionosphere waveguide are determined particularly through dawn and dusk using phase and amplitude measurements of man-made signals propagating below the ionospheric D region. For the first time variations of “Wait” height and sharpness parameters, H' and β, have been determined for dawn and dusk conditions. These measurements provide observational data to constrain D region modeling efforts, extending the capabilities of VLF propagation monitoring for geophysical phenomena such as lightning, solar flares, and energetic particle precipitation. At mid-latitudes, H' varied from ∼85 km at night, then, starting from solar zenith angle (SZA) ∼ −97.5°, rapidly down to ∼73 km at dawn (SZA = −90°), then back up to ∼78 km at SZA ∼ −75° and then down to the appropriate noon value for the latitude (and season). In contrast, from noon through dusk to night, H' varied essentially monotonically from ∼70 to 75 km through ∼80 to ∼85 km. At low latitudes no dawn minimum in H' was observed, due to the reduced effect of galactic cosmic rays (GCR). Sharpness, β, varied from its nighttime value of ∼0.6 km−1 down to a minimum of ∼0.25 km−1 at SZA ∼85° near dusk or ∼75° near dawn, rising again to (SZA-dependent) noon values of ∼0.35–0.5 km−1. The results are interpreted through the geophysical effects controlling D region electrons, including the daytime dominant role of solar Lyman-α from low to mid-latitudes, and the greater role of GCR at increasingly higher mid-latitudes.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1029/2024JA033610 |
ISSN: | 2169-9380 |
Additional Keywords: | D-region dawn and dusk, electron number densities, D-region height and sharpness, solar zenith angle, galactic cosmic rays, solar lyman-alpha |
Date made live: | 10 Apr 2025 13:37 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/539246 |
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