Low-frequency wave characteristics in the upstream and downstream regime of the terrestrial bow shock

Details Low-frequency wave characteristics in the upstream and downstream regime of the terrestrial bow shock Low-frequency wave characteristics in the upstream and downstream regime of the terrestrial bow shock

Jan 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgra..11101203n&link_type=abstract

Journal of Geophysical Research, Volume 111, Issue A1, CiteID A01203

Physics

17

Interplanetary Physics: Plasma Waves And Turbulence, Interplanetary Physics: Planetary Bow Shocks, Magnetospheric Physics: Plasma Waves And Instabilities (2471), Electromagnetics: Wave Propagation (2487, 3285, 4275, 4455, 6934)

Scientific paper

Collisionless shocks in space are accompanied by the low-frequency waves of the magnetic field both upstream and downstream of the shock. However, characteristics of these waves in the plasma rest frame are poorly understood, since spatial scale such as wavelength is hardly determined using single or at best two spacecraft observations. Taking advantage of multipoint measurements of the Cluster spacecraft, we present a statistical study to reveal the rest frame properties of the waves in the terrestrial bow shock environment such as frequencies, wave numbers, phase velocities, propagation directions, polarization and transport ratios for the quasi-parallel and the quasi-perpendicular shock regimes and in the upstream region, the outer, the middle, and the inner magnetosheath. We find that the quasi-parallel shock upstream waves (or the foreshock waves) exhibit properties of the fast mode wave excited by the ion beam instability. Upstream of the quasi-perpendicular shock the waves also exhibit similar properties to the foreshock waves, but the wave mode identification needs further investigations. In the magnetosheath the waves exhibit properties which are persistent from the outer to the inner magnetosheath. They can be interpreted as the mirror mode coupled to the plasma inhomogeneity or as the slow mode. We also find an organization in the wave propagation pattern that the upstream waves propagate toward upstream, while the magnetosheath waves propagate toward the flank region and toward the magnetopause. It is concluded that wave properties are different between the upstream and the downstream regions, but they are similar between the quasi-parallel and the quasi-perpendicular shock regimes, suggesting that the upstream waves are not transmitted to the downstream region across the shock and that the downstream waves do not depend on the shock angle (between the upstream magnetic field and the shock normal direction).

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