“…As a result, solar proxies well‐correlated with solar EUV irradiance which can be measured from the ground, such as F10.7 (Tapping, 2013), have seen regular usage due to their operational availability, and are routinely used as inputs for Ionosphere‐Thermosphere models such as NRLMSISE 2.0 (Emmert et al., 2021) and Thermosphere Ionosphere Electrodynamics General Circulation Model (Cai et al., 2022). While these solar proxies have demonstrated applicability in downstream modeling for representing thermospheric and ionospheric climatology, they suffer from some important limitations, including: - Each solar index is best described as a proxy for solar processes occurring either in the photosphere, chromosphere, transition region, corona, or a combination of some of these regions, limiting their ability to capture the entire swath of variation throughout the entire EUV range (To et al., 2023).
- The emissions most strongly correlated with each solar index are absorbed in different regions of the thermosphere and mesosphere, resulting in either increasingly complex parameterization for their ingestion into atmospheric models and non‐trivial impacts on quantification of uncertainty in derived thermospheric temperatures and densities (Thayer et al., 2021).
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