Solar Terminator Waves Revealed as Dominant Features of Upper Thermospheric Density

Abstract Observations of solar terminator waves (STWs) in thermospheric mass density (TMD) measurements above 500 km reveal STWs as dominant features of the upper thermosphere. While previous investigations have shown that STWs in the middle‐lower thermosphere have amplitudes on the order of 6%–8% of the background TMD in that region, this study shows that STWs exhibit a striking amplification with altitude, producing density perturbations of up to a factor of two near 500 km. The study analyzes STWs in TMD data across altitude, solar cycle, and both solstices, leveraging a direct comparative methodology with Challenging Minisatellite Payload, Gravity Recovery and Climate Experiment Follow‐On, and High‐Accuracy Satellite Drag Model. The first detection of a dawn STW with a magnitude comparable to dusk is made near 500 km, contrasting the asymmetry seen at lower altitudes. The newfound prominence of STWs highlights the need for further research into their generation mechanisms, role in geophysical variability, and broader implications for thermospheric modeling and spacecraft operations.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-05-31
DOI
https://doi.org/10.1029/2025gl115612
Citations
1
Primary Topic
Solar and Space Plasma Dynamics
Type
article
Field-Weighted Citation Impact
1.15

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article

Solar Terminator Waves Revealed as Dominant Features of Upper Thermospheric Density

David Fitzpatrick, Marcin Pilinski, S. E. Palo, E. K. Sutton
1 citations
Geophysical Research Letters
Solar and Space Plasma Dynamics
1.15
article

Solar Terminator Waves Revealed as Dominant Features of Upper Thermospheric Density

David Fitzpatrick, Marcin Pilinski, S. E. Palo, E. K. Sutton
article en
1 citations

Abstract

Abstract Observations of solar terminator waves (STWs) in thermospheric mass density (TMD) measurements above 500 km reveal STWs as dominant features of the upper thermosphere. While previous investigations have shown that STWs in the middle‐lower thermosphere have amplitudes on the order of 6%–8% of the background TMD in that region, this study shows that STWs exhibit a striking amplification with altitude, producing density perturbations of up to a factor of two near 500 km. The study analyzes STWs in TMD data across altitude, solar cycle, and both solstices, leveraging a direct comparative methodology with Challenging Minisatellite Payload, Gravity Recovery and Climate Experiment Follow‐On, and High‐Accuracy Satellite Drag Model. The first detection of a dawn STW with a magnitude comparable to dusk is made near 500 km, contrasting the asymmetry seen at lower altitudes. The newfound prominence of STWs highlights the need for further research into their generation mechanisms, role in geophysical variability, and broader implications for thermospheric modeling and spacecraft operations.

Geophysical Research LettersVol. 52(11)
University of Colorado Boulder (US), Laboratory for Atmospheric and Space Physics (US)
National Science Foundation, National Aeronautics and Space Administration, Nuclear Safety and Security Commission, National Oceanic and Atmospheric Administration
Openalex Percentile: Top 19%
Solar and Space Plasma Dynamics
1.15
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