Modeling studies of the impact of high-speed streams and co-rotating interaction regions on the thermosphere-ionosphere

Changes in the thermosphere‐ionosphere system caused by high‐speed streams in the solar wind, and the co‐rotating interaction regions they engender, are studied using a combination of model simulations and data analysis. The magnetospheric responses to these structures and consequent ionospheric drivers are simulated using the numerical Coupled Magnetosphere‐Ionosphere‐Thermosphere model and the empirical Weimer 2005 model, finding that the interplanetary magnetic field (IMF) is more important than solar wind speed and density per se in controlling magnetosphere‐ionosphere coupling. The NCAR Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model is then employed to calculate neutral density, nitric oxide cooling, and electron density, for comparison to space‐based measurements from the STAR instrument on the CHAMP satellite, the SABER instrument on the TIMED satellite, and GPS occultations from the COSMIC mission, respectively. The recurrent, periodic changes observed under solar minimum conditions during 2008, and particularly during the Whole Heliospheric Interval (March–April of 2008), are simulated by the model and compared to these measurements. Numerical experiments were conducted to elucidate the mechanisms of solar wind and IMF forcing, setting the solar wind speed and density to nominal values, smoothing the IMF, and also setting it to zero. The results confirm the importance of IMF variations, particularly its north‐south component (Bz), but also show that when the average Bzvalues are negative (southward), the interaction with increased solar wind speed amplifies the magnetosphere‐ionosphere‐thermosphere response. Conversely, during events whenBz is on average positive (northward), even large increases in solar wind speed have small effects on the system. Key Points Thermosphere‐ionosphere impacts during HSS/CIR are mostly caused by IMF changes Amplification due to solar wind speed is most significant when Bz is southward Numerical modeling describes the diversity of thermosphere‐ionosphere response