Storm time evolution of the outer radiation belt: Transport and losses
By A. Y. Ukhorskiy, Brian J. Anderson, P. Brandt, N. Tsyganenko. 2006
157 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/9ba08de57178f8e6999e87af4861069c8dbb2977
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Citations in the corpus
- Radiation Belt Environment model: Application to space weather nowcasting (2008, methodology): “Using a test particle approach, Ukhorskiy et al. [2006] simulated the evolution of outer belt electrons during the magnetic storm of 7 September 2002.”
- Global distributions of suprathermal electrons observed on THEMIS and potential mechanisms for access into the plasmasphere (2010, background): “…possibly due to pitch angle scattering by chorus waves and electrostatic Electron Cyclotron Harmonic (ECH) waves [e.g., Horne et al., 2003; Ni, et al., 2008; Su et al., 2009; Thorne et al., 2010] and magnetopause shadowing [e.g., Li et al., 1997; Desorgher et al., 2000; Ukhorskiy et al., 2006].”
- Radiation Belt Storm Probes Ion Composition Experiment (RBSPICE) (2013, background): “This effect can explain rapid depletion of electron fluxes over a broad region of the outer electron belt during storm main phase (e.g., Ukhorskiy et al. 2006; Turner et al. 2012).”
- Space Weather Effects in the Earth’s Radiation Belts (2018, background): “…(Gkioulidou et al. 2014), thereby diamagnetically expanding electron drift orbits to a point where magnetopause shadowing (West et al. 1972) can have a greater effect on the core population (Ukhorskiy et al. 2006) and lead to dramatic dropout features in the observations (Shprits et al. 2006).”
- Use of POES SEM-2 observations to examine radiation belt dynamics and energetic electron precipitation into the atmosphere (2010, background): “…fraction of all of the particles lost are precipitated into the atmosphere [Lorentzen et al., 2001; Horne, 2002; Friedel et al., 2002; Clilverd et al., 2006], although storm‐time nonadiabatic magnetic field changes also lead to losses through magnetopause shadowing [e.g., Ukhorskiy et al., 2006].”
- On the storm‐time evolution of relativistic electron phase space density in Earth's outer radiation belt (2013, background): “This happens due to sudden inward motion of the magnetopause in response to increased solar wind dynamic pressure and is known as magnetopause shadowing [e.g., Ukhorskiy et al., 2006].”
- Explaining sudden losses of outer radiation belt electrons during geomagnetic storms (2012, background): “Losses to the magnetopause can occur through magnetopause ‘shadowing&rsquo”