 |
| Titel |
A case study on generation mechanisms of a sporadic sodium layer above Tromsø (69.6° N) during a night of high auroral activity |
| VerfasserIn |
T. Takahashi, S. Nozawa, T. T. Tsuda, Y. Ogawa, N. Saito, T. Hidemori, T. D. Kawahara, C. Hall, H. Fujiwara, N. Matuura, A. Brekke, M. Tsutsumi, S. Wada, T. Kawabata, S. Oyama, R. Fujii |
| Medientyp |
Artikel
|
| Sprache |
Englisch
|
| ISSN |
0992-7689
|
| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 33, no. 8 ; Nr. 33, no. 8 (2015-08-05), S.941-953 |
| Datensatznummer |
250121228
|
| Publikation (Nr.) |
 copernicus.org/angeo-33-941-2015.pdf |
|
|
|
|
|
| Zusammenfassung |
| We have quantitatively evaluated generation mechanisms of a sporadic sodium
layer (SSL) based on observational data obtained by multiple instruments at a
high-latitude station: Ramfjordmoen, Tromsø, Norway (69.6° N,
19.2° E). The sodium lidar observed an SSL at 21:18 UT on 22
January 2012. The SSL was observed for 18 min, with a maximum sodium density
of about 1.9 × 1010 m−3 at 93 km with a 1.1 km
thickness. The European Incoherent Scatter (EISCAT) UHF radar observed a sporadic E layer (Es layer) above
90 km from 20:00 to 23:00 UT. After 20:00 UT, the Es layer gradually
descended and reached 94 km at 21:18 UT when the SSL appeared at the same
altitude. In this event, considering the abundance of sodium ions (10 %
or less), the Es layer could provide only about 37 % or less of the
sodium atoms to the SSL. We have investigated a temporal development of the
normal sodium ion layer with a consideration of chemical reactions and the
effect of the (southwestward) electric field using observational values of
the neutral temperature, electron density, horizontal neutral wind, and
electric field. This calculation has shown that those processes, including
contributions of the Es layer, would provide about 88 % of sodium atoms of
the SSL. The effects of meteor absorption and auroral particle sputtering appear
to be less important. Therefore, we have concluded that the major source of
the SSL was sodium ions in a normal sodium ion layer. Two processes – namely
the downward transportation of sodium ions from a normal sodium ion layer due
to the electric field and the additional supply of sodium ions from the
Es layer under relatively high electron density conditions (i.e., in the
Es layer) – played a major role in generating the SSL in this event.
Furthermore, we have found that the SSL was located in a lower-temperature
region and that the temperature inside the SSL did not show any remarkable
temperature enhancements. |
| |
|
| Teil von |
|
|
|
|
|
|
|
|