- 1Finnish Geospatial Research Institute (FGI), National Land Survey of Finland (NLS), Department of Navigation and Positioning, Espoo, Finland (fabricio.dossantosprol@nls.fi)
- 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via di Vigna Murata 605, 00143 Rome, Italy
- 3Department of Earth and Environmental Sciences, Ludwig Maximilian University of Munich (LMU), Theresienstraße 41, 80333 Munich, Germany
- 4GFZ Helmholtz Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
The dynamics of the ionosphere and plasmasphere are strongly coupled: the ionosphere refills the plasmasphere on the dayside, while plasmaspheric particles help sustain the ionosphere at night. The NeQuick model, for instance, extrapolates ionospheric dynamics into the plasmasphere using parameters anchored in the F2-layer. However, despite these strong coupling processes, empirical models can benefit from treating these "spheres" as distinct regions. In this work, we propose a new formulation for the NeQuick model, which considers the plasmasphere as a layer entirely independent of ionospheric parameters. This adjustment led to significant improvements, partially resolving previous model underestimations and preserving a more realistic plasmaspheric structure along geomagnetic field lines. Based on extensive validation using data from 2008 to 2024, the revised NeQuick model demonstrated improvements ranging from 28% to 40%, depending on solar activity. These results suggest that modeling the ionosphere and plasmasphere as independent layers is a viable solution for improving both accuracy and the representation of plasma structures.
How to cite: Prol, F., Pignalberi, A., and Smirnov, A.: Improving NeQuick Model Connection between the Topside Ionosphere and Plasmasphere, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-13727, https://doi.org/10.5194/egusphere-egu26-13727, 2026.