Geotail observations of the low‐latitude boundary layer (LLBL) in the near–Earth tail flanks
are reported. Cold‐dense stagnant ions, which are likely to be of the magnetosheath origin …

GEOTAIL observations of the low-latitude boundary layer (LLBL) in the tail-flanks show that
they are the region where the cold-dense plasma appears with stagnant flow signatures …

Energetic (0.1‐16 keV/e) ion data from the Plasma Composition Experiment on the ISEE 1
spacecraft show that Earth's plasma sheet (inside of 23 RE) always has a large population of …

To further our understanding of the solar wind entry across the magnetopause under
northward IMF, we perform a case study of a duskside Kelvin-Helmholtz (KH) vortex event …

1. Introduction Significant controversy persists regarding the regions in the magnetotail to
which the discrete and diffuse aurorae map (FELDSTEIN and GALPERIN, 1985; SANDAHL …

In search for clues towards the understanding of the cold plasma sheet formation under
northward IMF, we study the temperature anisotropy of the two-component protons in the …

Data from an all‐sky imaging photometer (427.8 and 630.0 nm) in the central polar cap, the
IMP 8 and ISEE 2 satellites in the solar wind, and the DMSP F6, F7, and F8 satellites in the …

The near‐Earth plasma sheet becomes cold and dense under northward interplanetary
magnetic field (IMF) condition, which suggests efficient solar wind plasma entry into the …

Through the effort to obtain clues toward understanding of transport of cold plasma in the
near-Earth magnetotail under northward IMF, we find that two-component protons are …

Geotail observations of the low-latitude boundary layer (LLBL) in the tail-flanks show that it is
where the cold-dense ions appear with stagnant flow signatures accompanied by bi …