Some features of electron density behaviour in the high latitude D-region derived from in situ measurements

Details Some features of electron density behaviour in the high latitude D-region derived from in situ measurements Some features of electron density behaviour in the high latitude D-region derived from in situ measurements

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003jastp..65..417d&link_type=abstract

Journal of Atmospheric and Solar-Terrestrial Physics, Volume 65, Issue 4, p. 417-427.

Physics

1

Scientific paper

A large database of rocket measurements of the D-region electron concentration has been studied. The data were obtained at four sites in the Antarctic (Molodezhnaya and Syowa) and Arctic (Heiss Island, and And/øya/Kiruna). The electron densities were analysed in terms of their variations with solar zenith angle, geomagnetic activity and atmospheric temperature. We found that there is a particle ionisation source in the auroral oval even in quiet conditions. The energy of the particles is such, that they penetrate down to 85km, are partially absorbed between 85 and 80km but do not penetrate (are completely absorbed) below 75km. Analysis of the dependence of the electron concentration [e] on the daily sum of Kp indices, /∑Kp, shows that at all heights considered there is an increase of [e] with /∑Kp up to some saturation value of /∑Kp and beyond this level [e] is either constant (with large scatter of the data) or even decreases. This indicates that when the auroral oval expands with increasing geomagnetic activity, a particular station may move from a position outside or at the boundary of the oval, to a position inside the polar cap. An attempt is made to find the temperature dependence of the electron concentration. It is found that [e] at 75 and 80km increases with temperature /T. Analysis of the flights conducted during noctilucent cloud (NLC) events at And/øya/Kiruna reveals a strong dependence of [e] on /∑Kp at 80 and 85km. This dependence is stronger and better defined than that for the entire data set. This may be explained by the low mesopause temperatures observed in summer when NLC occur. A comparison of the electron density data sets with empirical and theoretical models is presented and during quiet magnetic conditions a good agreement with mid-latitude models is found.

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