Observation and theory of Pc 5 waves with harmonically related transverse and compressional components

The properties of 23 magnetic pulsation events observed by the AMPTE CCE spacecraft are studied. These events are selected on the basis of the field magnitude which oscillated at the second harmonic of a simultaneously present transverse oscillation. The events have a second harmonic period of 80–600 s (roughly the Pc 5 range), are observed in cluster in the dawn (0300–0800 magnetic local time, MLT) and dusk (1600–2100 MLT) sectors, and are localized near the magnetic equator. Although the azimuthal wave number, m, estimated from an ion finite Larmor radius effect, is generally large (|m| ∼ 50), there is a marked difference between the events observed in the dawn and dusk sectors. In the dawn sector the waves have low frequencies (1–5 mHz), indicate left-hand polarization with respect to the ambient magnetic field, and propagate eastward with respect to the spacecraft. In the dusk sector the waves have high frequencies (5–15 mHz), indicate right-hand polarization, and propagate westward. We suggest that the waves are all westward propagating in the plasma rest frame and that local-time-dependent Doppler shift is the reason for the local time dependence of the wave properties. The drift mirror instability is considered to be the mechanism for exciting the westward propagating waves. An analytical formula for the ion flux oscillations is derived on the basis of the nonlinear gyrokinetic theory. The observed correlation between the ion flux and the parallel magnetic field perturbation δB∥ can be adequately explained with this analytical formula.

[1]  A. Hasegawa,et al.  Theory of drift mirror instability , 2013 .

[2]  L. Kistler,et al.  Magnetospheric ULF waves observed during the major magnetospheric compression of November 1, 1984 , 1988 .

[3]  A. Hasegawa,et al.  On magnetospheric hydromagnetic waves excited by energetic ring‐current particles , 1988 .

[4]  M. Kivelson,et al.  An unambiguous determination of the propagation of a compressional Pc 5 wave , 1988 .

[5]  E. Amata,et al.  CURVATURE-DRIVEN DRIFT MIRROR INSTABILITY IN THE MAGNETOSPHERE , 1988 .

[6]  Hisao Yamagishi,et al.  Eastward propagation of PC4‐5 range CNA pulsations in the morning sector observed with scanning narrow beam riometer at L=6.1 , 1988 .

[7]  L. Kistler,et al.  An eastward propagating compressional Pc 5 wave observed by AMPTE/CCE in the postmidnight sector. [Active Magnetospheric Particle Tracer Explorers , 1987 .

[8]  K. Glassmeier,et al.  Plasma and field observations of a compressional Pc 5 wave event , 1987 .

[9]  C. Lin,et al.  Eigenmode analysis of compressional waves in the magnetosphere , 1987 .

[10]  E. Amata,et al.  Field-Aligned Structure of the Storm Time Pc 5 Wave of November 14-15, 1979, , 1987 .

[11]  M. Acuna,et al.  A model for the harmonic of compressional Pc 5 waves , 1987 .

[12]  T. Higuchi,et al.  Harmonic structure of compressional Pc5 pulsations at synchronous orbit , 1986 .

[13]  E. Nielsen,et al.  STARE and SABRE observations of a Pc 5 pulsation with large azimuthal wave number during a storm period , 1985 .

[14]  C. Lin,et al.  Azimuthal propagation of storm time Pc 5 waves observed simultaneously by geostationary satellites GOES 2 and GOES 3 , 1985 .

[15]  C. Russell,et al.  ISEE 1 and 2 observation of the spatial structure of a compressional Pc5 wave , 1985 .

[16]  S. Krimigis,et al.  The Medium-Energy Particle Analyzer (MEPA) on the AMPTE CCE Spacecraft , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[17]  G. Gloeckler,et al.  The Charge-Energy-Mass Spectrometer for 0.3-300 keV/e Ions on the AMPTE CCE , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[18]  M. Acuna,et al.  The AMPTE CCE Magnetic Field Experiment , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[19]  M. Kivelson,et al.  Charged particle behavior in low‐frequency geomagnetic pulsations: 4. Compressional waves , 1985 .

[20]  D. Baker,et al.  Azimuthal propagation and frequency characteristic of compressional Pc 5 waves observed at geostationary orbit , 1985 .

[21]  K. Glassmeier,et al.  Ground-satellite coordinated study of the April 5, 1979 events: flux variations of energetic particles and associated magnetic pulsations , 1984 .

[22]  A. Walker,et al.  Stare observations of an eastward propagating Pc5 pulsation with large azimuthal wavenumber , 1984 .

[23]  T. Araki,et al.  Long‐duration Pc5 pulsations observed by geostationary satellites , 1983 .

[24]  R. Greenwald,et al.  STARE and GEOS 2 observations of a storm time Pc 5 ULF pulsation , 1982 .

[25]  E. Nielsen,et al.  STARE Observations of a Pc 5 pulsation with large azimuthal wave number , 1982 .

[26]  E. Frieman,et al.  Nonlinear gyrokinetic equations for low-frequency electromagnetic waves in general plasma equilibria , 1981 .

[27]  E. Amata,et al.  Observations of quasi‐periodic flux variations of energetic ions and electrons associated with Pc 5 geomagnetic pulsations , 1981 .

[28]  R. McPherron,et al.  A SEASONAL CHANGE IN THE EFFECT OF FIELD-ALIGNED CURRENTS , 1980 .

[29]  P. C. Hedgecock Giant PC5 pulsations in the outer magnetosphere: A survey of HEOS-1 data , 1976 .

[30]  David J. Southwood,et al.  A general approach to low‐frequency instability in the ring current plasma , 1976 .

[31]  R. McPherron,et al.  Statistical characteristics of storm‐associated Pc 5 micropulsations observed at the synchronous equatorial orbit , 1972 .

[32]  A. Hasegawa,et al.  Drift mirror instability in the magnetosphere: Particle and field oscillations and electron heating , 1969 .

[33]  L. R. Davis,et al.  Resonant vibration of the magnetosphere observed from Explorer 26 , 1969 .

[34]  C. Russell,et al.  Some remarks on the position and shape of the neutral sheet , 1967 .

[35]  J. V. Evans,et al.  Empirical models for the plasma convection at high latitudes from Millstone Hill observations , 1987 .

[36]  M. Rosenbluth,et al.  Finite Larmor radius stability theory of ELMO Bumpy Torus plasmas , 1983 .

[37]  A. Hasegawa Drift Mirror Instability in the Magnetosphere , 1969 .

[38]  L. R. Davis,et al.  Acceleration of trapped particles during a magnetic storm on April 18, 1965 , 1968 .