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| Titel |
Vertical circulation and thermospheric composition: a modelling study |
| VerfasserIn |
H. Rishbeth, I. C. F. Müller-Wodarg |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
0992-7689
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| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 17, no. 6 ; Nr. 17, no. 6, S.794-805 |
| Datensatznummer |
250013777
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| Publikation (Nr.) |
 copernicus.org/angeo-17-794-1999.pdf |
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| Zusammenfassung |
The coupled
thermosphere-ionosphere-plasmasphere model CTIP is used to study the global
three-dimensional circulation and its effect on neutral composition in the
midlatitude F-layer. At equinox, the vertical air motion is basically up by day,
down by night, and the atomic oxygen/molecular nitrogen [O/N2]
concentration ratio is symmetrical about the equator. At solstice there is a
summer-to-winter flow of air, with downwelling at subauroral latitudes in winter
that produces regions of large [O/N2] ratio. Because the
thermospheric circulation is influenced by the high-latitude energy inputs,
which are related to the geometry of the Earth's magnetic field, the latitude of
the downwelling regions varies with longitude. The downwelling regions give rise
to large F2-layer electron densities when they are sunlit, but not when they are
in darkness, with implications for the distribution of seasonal and semiannual
variations of the F2-layer. It is also found that the vertical distributions of
O and N2 may depart appreciably from diffusive equilibrium at heights
up to about 160 km, especially in the summer hemisphere where there is strong
upwelling.
Atmospheric composition and structure
(thermosphere · composition and chemistry) · Ionosphere (ionosphere ·
atmosphere interactions) |
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