Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects

By J. Oberheide, Jeff Forbes, K. Häusler, Qian Wu, Sean Bruinsma. 2009

240 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/0c308ca8ecc06d009de5f207d0c5577b1a815cb7

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. R. Akmaev
2. Jeff Forbes
3. Han-Li Liu
4. H. Liu
5. J. Oberheide
6. N. Pedatella
7. Astrid Maute
8. Xiaoli Zhang

In Oceanography

1. H. Liu
2. N. Pedatella
3. Xiaoli Zhang
4. Han-Li Liu
5. Jeff Forbes
6. R. Roble
7. J. Oberheide
8. Sean Bruinsma

Citations in the corpus

• Variability and predictability of the space environment as related to lower atmosphere forcing (2016, background): “Observations have shown that tidal signals can extend into the upper thermosphere, including the ionospheric dynamo region [e.g., Häusler et al., 2007; Häusler and Lühr, 2009; Forbes et al., 2008, 2009; Oberheide et al., 2009; Häusler et al., 2010], in spite of the strong molecular damping of the wa”
• Development and Validation of the Whole Atmosphere Community Climate Model With Thermosphere and Ionosphere Extension (WACCM‐X 2.0) (2018, methodology): “This is consistent with the DE3 at this altitude derived from Hough model extension (HME) fitting of SABER and TIDI measurements (Oberheide et al., 2009).”
• Wave-driven variability in the ionosphere-thermosphere-mesosphere system from TIMED observations: What contributes to the wave 4 ? (2011, methodology): “Emphasis is on the year 2008 because the DE3 contributions should be largest then, owing to the reduced tidal dissipation in the thermosphere during solar minimum [ Oberheide et al., 2009 ].”
• Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, unknown): “Upward propagating tides from the lower atmosphere are not sensitive to the solar cycle (e.g., Oberheide et al. 2009).”
• Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, unknown): “X drop to 4–6 ms−1, consistent with the DE3 zonal wind derived from the measurements by the Challenging Minisatellite Payload (CHAMP) satellite [Oberheide et al., 2009; Häusler et al., 2010].”
• Internal wave coupling processes in Earth's atmosphere (2014, unknown): “Oberheide et al. (2009) have studied the question of how much of the tidal signatures propagates directly to the upper atmosphere.”
• WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “, 2010] are also in good agreement with SABER and TIMED Doppler Interferometer (TIDI) observations in the MLT and with semiempirical modeling of upward propagation based on these observations higher in the thermosphere [Oberheide et al., 2009].”