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Why We Need Global Observations

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Magnetospheric Physics

Abstract

Since its initiation with the remarkable discovery of the Van Allen radiation belts, the field of magnetospheric physics has been characterized by a continuing collection of data from in-situ satellite observing stations. The synthesis of these and ground-based observations has yielded an intriguing picture of a basic cosmological building block, the magnetosphere. Because of the time/space separation inherent in magnetospheric observations, this view necessarily is schematic in nature and our knowledge of global behavior is correspondingly incomplete. Since both local and global perspectives must be combined to understand such a complex physical system, the lack of appropriate global magnetospheric observations represents a serious impediment towards obtaining an understanding of magnetospheric dynamics. From the use of ground-based station networks to the advent of satellite auroral images, the drive for global knowledge has been relentless and has always delivered new and unexpected perspectives of the structures and phenomena being studied. This need for an overall perspective has brought us to the point of now being able to globally image the particle populations of the magnetosphere. This, combined with existing large-scale observations, provides for the first time, the capability of observing the magnetosphere on a global basis. We expect that when this capability is realized, our concepts of the magnetosphere will be altered every bit as dramatically as Professor Van Allen’s discovery of the radiation belts changed our view of the space environment.

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References

  • Akasofu, S.-I., 1965, Dynamic morphology of Auroras, Space Sci. Rev., IV–4: 498.

    Google Scholar 

  • Akasofu, S.-I., and S. Chapman, 1972, Solar-Terrestrial Physics, Oxford University Press, Oxford.

    Google Scholar 

  • Baker, K.B., R.A. Greenwald, J.M. Rushoniemi, J.R. Dudeney, M. Pinnock, N. Mattin, and J.M. Leonard, 1989, PACE; Polar Anglo-American Experiment, EOS, 70: 785.

    Article  ADS  Google Scholar 

  • Broadfoot, A.L., 1986, Images of the magnetosphere and atmosphere: global effects (IMAGE), proposal for NASA Explorer Mission Concept Studies, Eds. D.J. Williams, L.A. Frank, A.L. Broadfoot, W.L. Imhoff, S.B. Mende, D.M. Hunten, R.G. Roble, and G.S. Siscoe.

    Google Scholar 

  • Frank, L.A., J.D. Craven, K.L. Ackerson, M.R. English, R.H. Eather, and R.L. Carovillano, 1981, Global auroral imaging instrumentation for the Dynamics Explorer Mission, Space Sci. Instr., 5: 369.

    ADS  Google Scholar 

  • Gloeckler, G., B. Wilken, W. Studemann, F.M. Ipavich, D. Hovestadt, D.C. Hamilton, and G. Kremser, 1985, First composition measurements of the bulk of the storm time ring current (1 to 300 keV/e) with AMPTE-CCE, Geophys. Res. Lett., 12: 325.

    Article  ADS  Google Scholar 

  • Gurnett, D.A., and U.S. Ivan, 1988, Plasma wave observations with the Dynamics Explorer 1 spacecraft, Rev. of Geophys., 88: 285.

    Article  ADS  Google Scholar 

  • Horwitz, J.L., R.H. Comfort, and C.R. Chappell, 1984, Thermal ion composition measurements of the formation of the new outer plasmasphere and double plasmapause during storm recovery phase, Geophys. Res. Lett., 11: 701.

    Article  ADS  Google Scholar 

  • Huff, R.L., W. Calvert, J.D. Craven, L.A. Frank, and D.A. Gurnett, 1988, Mapping of auroral kilometric radiation sources to the aurora, J. Geophys. Res., 10: 11–445.

    Google Scholar 

  • Iijima, T., T.A. Potemra, and L.J. Zanetti, 1988, Large-scale characteristics of magnetospheric equatorial currents, JHU Applied Physics Laboratory Preprint, 88–14.

    Google Scholar 

  • Keath, E.P., G.B. Andrews, A.F. Cheng, S.M. Krimigis, B.H. Mauk, D.G. Mitchell, and D.J. Williams, 1989, Instrumentation for energetic neutral atom imaging of magnetospheres, in Waite et al. (Eds.), Solar System Plasma Physics, Geophysical Monograph 54, American Geophysical Union, Washington D.C., p. 165.

    Chapter  Google Scholar 

  • McEntire, R.W., and D.G. Mitchell, 1989, Instrumentation for global magnetospheric imaging via energetic neutral atoms, in Waite et al. (Eds.), Solar System Plasma Physics, Geophysical Monograph 54, American Geophysical Union, Washington D.C., p. 69.

    Chapter  Google Scholar 

  • Newell, H.E., 1959, Capabilities for space research, J. Geophys. Res., 4: 1695.

    Article  ADS  Google Scholar 

  • Rairden, R.L., L.A. Frank, and J.D. Cruven, 1986, Geocoronal imaging with Dynamics Explorer, J. Geophys. Res., 91: 13613.

    Article  ADS  Google Scholar 

  • Roelof, E.C., D.G. Mitchell, and D.J. Williams, 1985, Energetic neutral atoms (E-50 keV) from the ring current: IMP 7/8 and ISEE 1, J. Geophys. Res., 90: 10991.

    Article  ADS  Google Scholar 

  • Roelof, E.C., 1987, Energetic neutral atom image of a storm-time ring current, Geophys. Res. Letters, 14: 652.

    Article  ADS  Google Scholar 

  • Roelof, E.C., and D.J. Williams, 1988, The terrestrial ring current: From in-situ measurements to global images using energetic neutral atoms, Johns Hopkins APL Technical Digest, 9: 144.

    ADS  Google Scholar 

  • Roelof, E.C., 1989, Remote sensing of the ring current using energetic neutral atoms, in press, Advances in Space Research,1989.

    Google Scholar 

  • Swift, D.W., R.W. Smith, and S.-I. Akasofu, 1989, Imaging the Earth’ s magnetosphere, Planet. Space Sci., 37: 379.

    Article  ADS  Google Scholar 

  • Van Allen, J.A., G.H. Ludwig, E.C. Ray, and C.E. Mcllwain, 1958, Observation of high intensity radiation by satellites, Jet Propul. 28: 588.

    Google Scholar 

  • Van Allen, J.A., C.E. Mcllwain, and G.H. Ludwig, 1959, J. Geophys.Res., 64: 271.

    Article  ADS  Google Scholar 

  • Van Allen, J.A., and L.A. Frank, 1959, Radiation around the Earth to a radial distance of 107,000 kilometers, Nature, 183: 430.

    Article  ADS  Google Scholar 

  • Vasyliunas, V.M., 1970, Mathematical models of magnetospheric convection and its coupling to the ionosphere, Particles and Fields in the Magnetosphere, Ed. B.M. McCormac, D. Reidel Pub. Co., p. 60.

    Chapter  Google Scholar 

  • Waite, J.H., J.L. Horwitz, and R.H. Comfort, 1984, Diffusive equilibrium distributions of He in the plasmasphere, Planet. Space Sci., 32: 611.

    Article  ADS  Google Scholar 

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© 1990 Springer Science+Business Media New York

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Williams, D.J. (1990). Why We Need Global Observations. In: Hultqvist, B., Fälthammar, CG. (eds) Magnetospheric Physics. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-7376-0_7

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  • DOI: https://doi.org/10.1007/978-1-4615-7376-0_7

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4615-7378-4

  • Online ISBN: 978-1-4615-7376-0

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