The quasi two-day wave (QTDW) at 82–97km altitude over Collm (51° N, 13° E) has been observed using a VHF meteor radar. The long-term mean amplitudes calculated using data between September 2004 and August 2014 show a strong summer maximum 5 and a much weaker winter maximum. In summer, the meridional amplitude is slightly larger than the zonal one with about 15ms°1 at 91 km height. Phase differences are slightly greater than 90° on an average. The periods of the summer QTDW vary between 43 and 52H during strong bursts, while in winter the periods tend to be more diffuse. On an average, the summer QTDW is amplified after a maximum of 10 zonal wind shear which is connected with the summer mesospheric jet and there is a possible correlation of the summer mean amplitudes with the backgound wind shear. QTDW amplitudes exhibit considerable inter-annual variability, however, a clear relation between the 11 year solar cycle and the QTDW is not found.
| Identifer | oai:union.ndltd.org:DRESDEN/oai:qucosa:de:qucosa:13321 |
| Date | January 2015 |
| Creators | Lilienthal, Friederike, Jacobi, Christoph |
| Contributors | Universität Leipzig |
| Publisher | European Geosciences Union |
| Source Sets | Hochschulschriftenserver (HSSS) der SLUB Dresden |
| Language | English |
| Detected Language | English |
| Type | doc-type:article, info:eu-repo/semantics/article, doc-type:Text |
| Source | Atmospheric chemistry and physics / Discussions 2015, 15: 9631–9659 |
| Rights | info:eu-repo/semantics/openAccess |
Page generated in 0.0024 seconds