Longitudinal variation of F region electron density and thermospheric zonal wind caused by atmospheric tides

By Hermann Lühr, K. Häusler, Claudia Stolle. 2007

149 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/089b42d70d1994b7f0c1e309b9a8c01ba2846aee

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. Jeff Forbes
2. J. Oberheide
3. R. Roble
4. M. E. Hagan
5. Dieter Bilitza
6. Astrid Maute
7. Bodo W. Reinisch
8. C. Mertens

In Oceanography

1. Eelco Doornbos
2. Dieter Bilitza
3. M. E. Hagan
4. R. Roble
5. Jeff Forbes
6. Lee-Anne McKinnell
7. J. Oberheide
8. Bodo W. Reinisch

Citations in the corpus

• The international reference ionosphere today and in the future (2011, methodology): “A good example is the recently discovered four maxima structure in the longitudinal variation of F-peak electron density and ionospheric electron content that was first observed with IMAGE/EUV observations (Immel et al. 2006), and then confirmed with data from CHAMP (Lühr et al. 2007) and TOPEX (Sch”
• The International Reference Ionosphere 2012 – a model of international collaboration (2014, methodology): “A good example is the recently discovered four maxima structure in the longitudinal variation of F-peak electron density and of ionospheric electron content that was first observed with IMAGE/EUV observations (Immel et al. 2006), and then confirmed with data from CHAMP (Lühr et al. 2007) and TOPEX (”
• Internal wave coupling processes in Earth's atmosphere (2014, unknown): “A number of researchers have provided evidences for tidal modulation of the low-latitude thermosphere (e.g., Lühr et al., 2007; Forbes et al., 2009; Liu et al., 2009; Oberheide et al., 2009).”
• Thermospheric Density and Wind Determination from Satellite Dynamics (2012, methodology): “[57] provides an algorithm, suitable for automated analysis on modern computers, that is more”
• Tidal propagation of deep tropical cloud signatures into the thermosphere from TIMED observations (2008, background): “The mechanism that couples the DE3 tidal signal into the F-region zonal wind is not yet understood [Lühr et al., 2007].”
• Tropospheric tidal effects on the middle and upper atmosphere (2009, background): “…1356 nm airglow brightness measurements [e.g., Sagawa et al., 2005; Immel et al., 2006; England et al., 2006b], electron density [Lin et al., 2007; Lühr et al., 2007], electric field [England et al., 2006a; Kil et al., 2007], electrojet [Lühr et al., 2008], and thermospheric wind data [Häusler…”
• Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, background): “…the longitudinal wavenumber-4 structure also occurred in other parameters such as the vertical ion drift velocity, the electron temperature, and even in the zonal neutral wind in the F region [Hartman and Heelis, 2007; Ren et al., 2008; Kil et al., 2007; Häusler et al., 2007; Lühr et al., 2007].”