Energetic and magnetosheath energy particle signatures of the low-latitude boundary layer at low altitudes near noon

Details Energetic and magnetosheath energy particle signatures of the low-latitude boundary layer at low altitudes near noon Energetic and magnetosheath energy particle signatures of the low-latitude boundary layer at low altitudes near noon

Sep 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992jgr....9713817r&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 97, no. A9, Sept. 1, 1992, p. 13,817-13,828. Research supported by Aerosp

Physics

13

Atmospheric Boundary Layer, Energetic Particles, Magnetosheath, Particle Precipitation, Angular Distribution, Field Aligned Currents, Noon, Particle Acceleration, Tropical Regions

Scientific paper

The energetic and magnetosheath energy particle signature of the low-latitude boundary layer (LBL) and its separation from the cusp are investigated using particle data from the polar-orbiting S3-3 satellite. The LBL and its boundaries, as determined from the energetic particles are compared with the LBL and boundaries determined from a modified set of low-energy plasma criteria based on Newell and Meng (NM, 1988, 1989). Excellent agreement was found in 68 percent of the 19 orbits where the LBL was identified by the energetic electron data. In 10 percent of the remaining orbits, the modified NM criteria did not provide numerical LBL identification, though a clear boundary region was visually identifiable in the data. For the remaining orbits, the modified NM criteria identified the LBL, but not its full latitudinal extent.

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