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Ring current asymmetry from global simulations using a high-resolution electric field model

By V.K. Jordanova, A. Boonsiriseth, R.M. Thorne and Y. Dotan
Year: 2003
DOI identifier: 10.1029/2003JA009993
OAI identifier: oai:eprints.lancs.ac.uk:35393
Provided by: Lancaster E-Prints

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Citations

  1. (1997). 98, edited by
  2. (1966). A general relation between the energy of trapped particles and the disturbance field over the Earth, doi
  3. (1997). A magnetic cloud containing prominence material: doi
  4. (2002). A model-derived storm time asymmetric ring current driven electric field description, doi
  5. (2001). A semiempirical equatorial mapping of AMIE convection electric potentials (MACEP) for the January 10, 1997, magnetic storm, doi
  6. (1973). A semiempirical model of large-scale magnetospheric electric fields, doi
  7. (1999). Analysis of early phase ring current recovery mechanisms during geomagnetic storms, doi
  8. (1992). Assimilative mapping of ionospheric electrodynamics, doi
  9. (1995). CEPPAD: Comprehensive energetic particle and pitch angle distribution experiment on Polar, Space Sci. doi
  10. (1998). Chen,J.,etal.,Cuspenergeticparticleevents:Implicationsforamajoracceleration region of the magnetosphere,
  11. (1996). Collisional losses of ring current ions, doi
  12. (2001). Comprehensive computational model of the Earth’s ring current, doi
  13. (1983). Convective growth rate of ion cyclotron waves in a H+-He+ and H+-He+-O+ plasma, doi
  14. (1998). Cusp energetic particle events: Implications for a major acceleration region of the magnetosphere, doi
  15. (1998). Dependence of the large-scale, inner magnetospheric electric field on geomagnetic activity, doi
  16. (1993). Effects of a high-density plasma sheet on ring current development during the November 2–6, doi
  17. (1984). Effects of energetic ions on electromagnetic ion cyclotron wave generation in the plasmapause region, doi
  18. (1996). Effects of heavy ions on the quasi-linear diffusion coefficients from resonant interactions with electromagnetic ion cyclotron waves, doi
  19. (2001). Energetic neutral atom images of a narrow flow channel from the plasma sheet: doi
  20. (1973). Energy and momentum theorems in magnetospheric processes, doi
  21. (1998). Experimental evidence on the role of the large spatial scale electric field in creating the ring current, doi
  22. (2001). First medium energy neutral atom (MENA) images of Earth’s magnetosphere during substorms and storm-time, doi
  23. (1986). Geocoronal imaging with Dynamics Explorer, doi
  24. (1998). Geoeffectiveness of three Wind magnetic clouds: A comparative study, doi
  25. (2001). Global dynamics of the plasmasphere and ring current during magnetic storms, doi
  26. (1997). Global energy deposition during the
  27. (1995). HYDRA—A 3-dimensional electron and ion hot plasma instrument for the POLAR spacecraft of the GGS mission, doi
  28. (1959). Hydromagnetic theory of geomagnetic storms, doi
  29. (2000). IMAGE mission overview, doi
  30. (2001). Imaging two geomagnetic storms in energetic neutral atoms, doi
  31. (1998). Ion cyclotron waves during a great magnetic storm observed by Freja double-probe electric field instrument, doi
  32. (1986). Ionospheric convection associated with discrete levels of particle precipitation, doi
  33. (1975). Isolated cold plasma regions: Observations and their relation to possible production mechanisms, doi
  34. (1997). Kinetic model of the ring current-atmosphere interactions, doi
  35. (1998). Large-scale geomagnetic effects of doi
  36. (2001). Low energy neutral atoms in the magnetosphere, doi
  37. (1995). magnetic cloud and accompanying storm activity: Ring current evolution, doi
  38. (1997). Modeling of ring current formation and decay: A review, in Magnetic Storms, doi
  39. Modeling ring current proton precipitation by electromagnetic ion cyclotron waves during the May 14–16, 1997, storm, doi
  40. (1996). Modeling the global magnetic field of the large-scale Birkeland current systems, doi
  41. (1997). Modulation of electromagnetic ion cyclotron instability due to interaction with ring current O + during magnetic storms, doi
  42. (1997). Modulation of electromagnetic ion cyclotron instability due to interaction with ring current O+ during magnetic storms, doi
  43. (1981). Quantitative simulation of a magnetic substorm: 1. Model logic and overview, doi
  44. (1997). Ring current activity during the early Bz doi
  45. (1996). Ring current development during storm main phase, doi
  46. (2000). Ring current dynamics during the 13–18 doi
  47. (2000). Ring current heating of the thermal electrons at solar maximum, doi
  48. (2002). SAPS: A new categorization for sub-auroral electric fields, Eos Trans. doi
  49. (1999). Simulation of off-equatorial ring current ion spectra measured by Polar for a moderate storm at solar minimum, doi
  50. (1994). Simulations of phase space distributions of storm time proton ring current, doi
  51. (1999). Testing electric field models using ring current ion energy spectra from the Equator-S ion composition (ESIC) instrument, doi
  52. (1987). The ionosphere as a fully adequate source of plasma for the Earth’s magnetosphere, doi
  53. (1998). The magnetospheric response to the CME passage of January 10–11, 1997, as seen at geosynchronous orbit, doi
  54. (1975). The motion of a proton in the equatorial magnetosphere, doi
  55. (1983). The quasi-static (slow-flow) region of the magnetosphere, in Solar-Terrestrial Physics, edited by doi
  56. (1997). The superdense plasma sheet: Plasmaspheric origin, solar-wind origin, or ionospheric origin?, doi
  57. (1995). The toroidal imaging mass-angle spectrograph (TIMAS) for the Polar mission, doi
  58. (1993). Two-dimensional model of the plasmasphere: Refilling time constants, doi

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