Lunar tide amplification during the January 2009 stratosphere warming event: Observations and theory

By Jeff Forbes, Xiaoli Zhang. 2012

134 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/188fd73df2d9bba89f9d9c3e23e3256393650097

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. H. Liu
2. N. Pedatella
3. Han-Li Liu
4. Y. Yamazaki
5. Y. Miyoshi
6. U. Langematz
7. Claudia Stolle
8. M. Hegglin

In Oceanography

1. H. Liu
2. U. Langematz
3. Han-Li Liu
4. A. Butler
5. D. Domeisen
6. N. Pedatella
7. C. Garfinkel

Citations in the corpus

• Variability and predictability of the space environment as related to lower atmosphere forcing (2016, background): “…mechanisms considered include nonlinearly interaction with the QSPWs, as well as changes in zonal mean zonal winds and tidal sources [e.g., Liu and Roble, 2002; Pancheva et al., 2009; Chang et al., 2009; Sridharan et al., 2012; Liu et al., 2010a; Fuller-Rowell et al., 2010; Forbes and Zhang, 2012].”
• September 2019 Antarctic Sudden Stratospheric Warming: Quasi‐6‐Day Wave Burst and Ionospheric Effects (2019, background): “Forbes and Zhang (2012) argued that the large semidiurnal lunar tide76 observed during the January 2009 SSW can arise from resonant amplification associated77 with the atmospheric Pekeris mode.”
• Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, unknown): “It has been shown that lunar atmospheric tides are subject to an amplification during stratospheric sudden warming events, which leads to enhanced lunar tidal effects in the ionosphere (Stening et al. 1997; Pedatella et al. 2012b; Forbes and Zhang 2012).”
• Sudden Stratospheric Warmings (2020, background): “The enhanced lunar tide is attributed to changes in the background zonal mean zonal winds, which shifts the Pekeris resonance mode of the atmosphere close to the frequency of the migrating semidiurnal lunar tide (Forbes & Zhang, 2012).”
• The influence of atmospheric tide and planetary wave variability during sudden stratosphere warmings on the low latitude ionosphere (2013, background): “Large changes in the vertical plasma drift velocity begin around day –10, which coincides with the onset of changes in the zonal mean atmosphere (Figure 2), and tidal variability in the MLT (Figures 3–5).”