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A missing dusk-side loss process in the terrestrial electron ring current.
Bernhard Haas1,2, Yuri Y Shprits3,4,5, Hayley J Allison3
1GFZ German Research Centre for Geosciences, Potsdam, Germany. bhaas@gfz-potsdam.de.
Earth's ring current models overestimate electron flux during geomagnetic storms. A missing loss process in the pre-midnight sector, likely due to wave-particle interactions, explains these discrepancies.
Area of Science:
- Space Physics
- Plasma Physics
- Geophysics
Background:
- The Earth's magnetic field generates a ring current from trapped charged particles.
- Ring current dynamics during geomagnetic storms are complex and not fully understood.
- Existing models show systematic overestimation of electron flux (10-50 keV) on the nightside during storm onset.
Purpose of the Study:
- To identify the cause of systematic overestimation of electron flux in current ring current models.
- To investigate missing loss processes affecting electron flux during geomagnetic storms.
- To improve the accuracy of ring current models.
Main Methods:
- Analysis of electron drift trajectories.
- Comparison of model predictions with satellite observations.
- Quantification of a previously unaccounted-for loss process.
Main Results:
- Existing ring current models overestimate nightside electron flux (10-50 keV) during storm onset.
- A significant electron loss process in the pre-midnight sector is identified.
- This loss process must operate at its theoretical maximum over a broad region to match observations.
Conclusions:
- A crucial electron loss mechanism is missing from current ring current models.
- Inaccuracies in modeling chorus wave interactions and the exclusion of electrostatic electron cyclotron harmonic wave scattering likely contribute to this missing loss.
- Accurate representation of these loss processes is essential for understanding geomagnetic storm dynamics.
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