Long-term trends of midlatitude horizontal mesosphere/lower thermosphere winds over four decades
<p>We analyse 43 years of mesosphere/lower thermosphere (MLT) horizontal winds obtained from a joint analysis of low frequency (LF) spaced receiver lower ionospheric drift measurements from late 1978 through 2008 and VHF meteor radar wind observations since summer 2004 at Collm (51.3<span c...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | deu |
| Published: |
Copernicus Publications
2023-12-01
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| Series: | Advances in Radio Science |
| Online Access: | https://ars.copernicus.org/articles/21/111/2023/ars-21-111-2023.pdf |
| Summary: | <p>We analyse 43 years of mesosphere/lower thermosphere (MLT) horizontal winds obtained from a joint analysis of low frequency (LF) spaced receiver lower ionospheric drift measurements from late 1978 through 2008 and VHF meteor radar wind observations since summer 2004 at Collm (51.3<span class="inline-formula"><sup>∘</sup></span> N, 13.0<span class="inline-formula"><sup>∘</sup></span> E). Due to limitations of the earlier LF measurements, we restrict ourselves to the analysis of monthly mean winds near 90 km, which represents the meteor peak height as well as mean LF reflection heights in the MLT. We observe mainly positive trends of the zonal prevailing wind throughout the year, while the meridional winds tend to decrease in magnitude in both summer and winter. Furthermore, there is a change in long-term trends around the late 1990s, which is most clearly visible in summer MLT winds. We compare these measurements with long-term partial reflection radar observations of winds at 81–85 km over Juliusruh (54.6<span class="inline-formula"><sup>∘</sup></span> N, 13.4<span class="inline-formula"><sup>∘</sup></span> E) since 1990, and find general qualitative agreement of trends except for summer. The latter can be explained by the different altitudes considered, and by the latitude dependence of the summer mesospheric jet.</p> |
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| ISSN: | 1684-9965 1684-9973 |