Abstract
This work presents the first simultaneous observations of Na and K between 120 and 150 km altitudes along with ionospheric tidal ion layers (TILs) obtained on 30 January 2006 data from Arecibo. The latter displays an average downward phase velocity of ∼14.7 ms-1. However, the neutral layers descend together at a much slower velocity of about ∼0.69 ms-1. This indicates that thermospheric atomic metal layers are not necessarily associated with TILs. The ratio of the average Na/K abundances in thermosphere is ∼35.5 as compared to 150 in the main layer (80-105 km). The long lifetimes of ions at ∼140 km implies that neutral layers cannot result from direct neutralization of metal ions in the TILs. We investigate different mechanisms that can deposit neutral atoms at thermospheric altitudes.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 10106-10112 |
| Number of pages | 7 |
| Journal | Geophysical Research Letters |
| Volume | 42 |
| Issue number | 23 |
| DOIs | |
| State | Published - Dec 16 2015 |
All Science Journal Classification (ASJC) codes
- Geophysics
- General Earth and Planetary Sciences
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