vix.ing · top · new · best · stats · spec

Impact of Solar Activity on the Ionosphere/Thermosphere during Geomagnetic Quiet Time for CTIPe and TIE-GCM

2017/01/23 by A. Fitzmaurice, Fitzmaurice, Anna, J. S. Shim +4
Biochemistry, Genetics and Molecular Biology · Physics and Astronomy · #Atmospheric and Oceanic Physics (physics.ao-ph) #FOS: Physical sciences #Geomagnetism and Paleomagnetism Studies #Ionosphere and magnetosphere dynamics #Solar and Space Plasma Dynamics #Space Physics (physics.space-ph)

paper · pdf · doi:10.48550/arxiv.1701.06525

openalex publication_date 2017/01/23 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28

Abstract

This study examines the impact that solar activity has on model results during geomagnetic quiet time for the ionosphere/thermosphere models: the Coupled Thermosphere Ionosphere Plasmasphere Electrodynamics Model (CTIPe) and the Thermosphere-Ionosphere-Electrodynamics General Circulation Model (TIE-GCM). Using varying F10.7 flux values as a measurement of solar activity, the models were run over a two-day period with the constant parameters Kp= 2, n= 3 cm3, and v= 400 km/s. Four F10.7 values (70, 110, 150, and 190) were selected based off of the average F10.7 values for geomagnetic quiet days across the current solar cycle. Our analysis of the model results showed that solar activity has the greatest effect on TEC output and the least effect on hmF2 and O/N2 output. Overall, TIE-GCM output tends to be higher than CTIPe, however, inconsistent values across the two-day CTIPe v3.1 output suggests that this model needs a longer warm-up period. When visually compared against observed data, CTIPe v3.2 performs the best, although all models greatly overestimated values for TEC. Analyses of models during geomagnetic quiet time are important in establishing a baseline which can be compared against storm data. An example of this was completed at the end of the study, using storm data obtained from Millstone Observatory on March 17, 2013. In this analysis, we found that TIE-GCM using the Weimer model to calculate the high-latitude electric potential provided more accurate results. Continued research in this area will be useful for understanding the impact of geomagnetic storms on the thermosphere/ionosphere.

Related