Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Compressional boundaries in the Earth's foreshock

Journal Article · · AIP Conference Proceedings
DOI:https://doi.org/10.1063/1.4811078· OSTI ID:22118617
;  [1];  [2];  [3]
  1. Instituto de Geofisica, Universidad Nacional Autonoma de Mexico, Coyoacan (Mexico)
  2. Institut de Recherche en Astrophysique et Planetologie, Toulouse (France)
  3. Solana Scientific Inc., Solana Beach, California (United States)
The terrestrial foreshock is a highly dynamic region populated by particles, waves and non-linear structures such as shocklets, SLAMS, hot flow anomalies, cavities and cavitons. Recently a new structure named foreshock compressional boundary (FCB) was reported in global hybrid simulations by Omidi et al. (2009). This structure represents a transition region that separates the highly disturbed foreshock plasma from pristine solar wind or from the region of field-aligned ion beams. The FCB is associated with a strong compression of magnetic field and density. Besides the enhancements in the field and density, the FCB also shows a region where these two quantities decrease below the ambient solar wind (SW) values. Here, we study a FCB observed by Cluster-1. This FCB shows that although sometimes FCBs are transition regions between the pristine solar wind plasma and the foreshock plasma, in this case the FCB separates a region with large amplitude waves from regions with high frequency (f{approx}1.7 Hz) small amplitude waves. We analyze the FCB properties, ion distributions inside them, and the waves near the structure.
OSTI ID:
22118617
Journal Information:
AIP Conference Proceedings, Journal Name: AIP Conference Proceedings Journal Issue: 1 Vol. 1539; ISSN APCPCS; ISSN 0094-243X
Country of Publication:
United States
Language:
English

Similar Records

Excitation of compressional waves and the formation of shocklets in the earth's foreshock
Journal Article · Fri May 01 00:00:00 EDT 1987 · J. Geophys. Res.; (United States) · OSTI ID:6349180

Formation of the wave compressional boundary in the earth's foreshock
Journal Article · Sat Oct 01 00:00:00 EDT 1988 · Journal of Geophysical Research; (United States) · OSTI ID:5876968

Observations of short large-amplitude magnetic structures at a quasi-parallel shock
Journal Article · Tue Mar 31 23:00:00 EST 1992 · Journal of Geophysical Research; (United States) · OSTI ID:5594879