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Quantifying Radiation Belt Electron Loss Processes at L < 4
S G Claudepierre1, Q Ma1,2, J Bortnik1
1Department of Atmospheric and Oceanic Sciences UCLA Los Angeles CA USA.
Electron lifetimes in Earth
Area of Science:
- Space Physics
- Plasma Physics
- Geophysics
Background:
- Earth's inner magnetosphere hosts energetic electrons.
- These electrons are lost through pitch-angle scattering.
- Understanding these loss processes is crucial for space weather prediction.
Purpose of the Study:
- To comprehensively analyze electron loss mechanisms in the inner magnetosphere.
- To quantify the timescales of electron decay due to various wave-particle interactions.
- To compare theoretical predictions with in-situ observations.
Main Methods:
- Utilized empirical models for wave spectra (hiss, lightning-generated whistler, VLF, EMIC waves).
- Computed pitch-angle diffusion coefficients and electron decay timescales.
- Incorporated Coulomb energy drag and accurate geomagnetic field models.
Main Results:
- Demonstrated good agreement between theoretical and observed electron lifetimes for L < 4.
- Showed sensitivity of decay timescales to plasmaspheric density models.
- Found Coulomb energy drag significantly improves agreement at L < 2.
Conclusions:
- Quasilinear pitch-angle scattering is a primary loss mechanism for inner magnetosphere electrons.
- Accurate modeling of plasmaspheric density and Coulomb losses is vital.
- Advanced geomagnetic field models refine lifetime calculations.
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