2022
DOI: 10.1007/978-3-030-82167-8
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Physics of Earth’s Radiation Belts

Abstract: use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made. The images or other third party material in this book are included in the book's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the book's Creative Commons license and your intended use is not permitt… Show more

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Cited by 17 publications
(16 citation statements)
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References 195 publications
(291 reference statements)
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“…Benacquista et al (2018) also supported the idea of flux increase on a large range of L* and decrease by only a limited number of CIR storms. Koskinen and Kilpua (2022) supported the idea of relativistic flux decrease during SIRs. The observations shown here are strictly during intense geomagnetic storms.…”
Section: Figuresupporting
confidence: 60%
“…Benacquista et al (2018) also supported the idea of flux increase on a large range of L* and decrease by only a limited number of CIR storms. Koskinen and Kilpua (2022) supported the idea of relativistic flux decrease during SIRs. The observations shown here are strictly during intense geomagnetic storms.…”
Section: Figuresupporting
confidence: 60%
“…Since, the ion's drift contour depends on the magnetic field configuration, the OP77Q external field model (Olson & Pfitzer, 1979) and IGRF internal field model (Finlay et al., 2010) have been obtained from the LANLGeoMag library and invoked in the calculation of L *. During a geomagnetic storm, the azimuthal asymmetry in the magnetospheric magnetic field increases and attains a non‐dipolar like configuration (Koskinen & Kilpua, 2022). When the guiding center of a stably trapped ion drifts around the Earth in a non‐dipolar magnetic field configuration, it traces a drift shell which is asymmetric around the dipole axis.…”
Section: Methodsmentioning
confidence: 99%
“…represents the bouncing-averaged efficient wave amplitude of the electric field, dτ = ds/V ∥ , and the integration is made along the dipole field line (Koskinen & Kilpua, 2022). Note that 〈δE ν 〉 b is in the same order with δE ν in Li et al (2021) and 〈δE ν 〉 b exp i(mϕ − ωt) varies with the same time phase as δE tν .…”
Section: Drift Resonance Mechanismmentioning
confidence: 99%
“…If the waves are compressional with a finite azimuthal number m , the Gyro‐Betatron mechanism operates and may play a major role in energy change (Li et al., 2021). So we can define the bouncing‐averaged energy change rate as: leftleft〈〉W˙〈〉trueW˙b=normaliμmγRELδEνbenormali(mϕωt) $\begin{array}{l}\left\langle \dot{W}\right\rangle \approx \left\langle {\dot{W}}_{b}\right\rangle =\mathrm{i}\frac{\mu m}{\gamma {R}_{E}L}{\left\langle \delta {E}_{\nu }\right\rangle }_{b}{\mathrm{e}}^{\mathrm{i}(m\phi -\omega t)}\hfill \end{array}$ where leftleftδEνb=1τb0τbδEνsin30.25emθnormaldτ $\begin{array}{l}{\left\langle \delta {E}_{\nu }\right\rangle }_{b}=\frac{1}{{\tau }_{b}}{\int }_{0}^{{\tau }_{b}}\frac{\delta {E}_{\nu }}{{\mathrm{sin}}^{3}\,\theta }\mathrm{d}\tau \hfill \end{array}$ represents the bouncing‐averaged efficient wave amplitude of the electric field, d τ = d s / V ∥ , and the integration is made along the dipole field line (Koskinen & Kilpua, 2022). Note that 〈 δE ν 〉 b is in the same order with δE ν in Li et al.…”
Section: Drift Resonance Mechanismmentioning
confidence: 99%