Troposphere-Thermosphere Tidal Coupling as Measured by the SABER Instrument on TIMED during July-September, 2002

By Jeff Forbes, J. Russell, S. Miyahara, Xiaoli Zhang, Scott E. Palo, M. Mlynczak, C. Mertens, M. E. Hagan. 2006

194 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/9be158613d44fcd195bd2eea2c6d1a31e9b11eba

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In Astronomy and Astrophysics

1. Jeff Forbes
2. J. Oberheide
3. M. Mlynczak
4. M. E. Hagan
5. J. Russell
6. R. Roble
7. Astrid Maute
8. T. Immel

In Atmospheric Science

1. M. Mlynczak
2. J. Russell
3. Jeff Forbes
4. T. Immel
5. J. Oberheide
6. M. E. Hagan
7. C. Hsiao
8. Jann‐Yenq Liu

Citations in the corpus

• Plausible effect of atmospheric tides on the equatorial ionosphere observed by the FORMOSAT‐3/COSMIC: Three‐dimensional electron density structures (2007, background): “…sun-synchronous) perspective, the E3 diurnal nonmigrating tide exhibits four lower thermospheric or E-region altitude maxima [e.g., Oberheide et al., 2003; Forbes et al., 2006] at the same longitudes of the four strong EIA zones shown in Figure 1 [e.g., Immel et al., 2006; England et al., 2006b].”
• Tropospheric tidal effects on the middle and upper atmosphere (2009, methodology): “Forbes et al. [2006] used a quasi-linear timedependent model after Miyahara and Wu [1989] to simulate a DE3 tide with an equatorial peak temperature amplitude of � 25K.”
• FORMOSAT-3/COSMIC observations of seasonal and longitudinal variations of equatorial ionization anomaly and its interhemispheric asymmetry during the solar minimum period (2009, background): “Immel et al. [2006], Forbes et al. [2006] , England et al. [2006], Liu and Watanabe [2008], and Kil et al. [2008] that the four-peaked longitudinal variation in EIA is brought about by the coupling from the diurnal E3 nonmigrating tidal winds originating from the lower atmosphere by altering the E ”
• Longitudinal structure of the equatorial ionosphere: Time evolution of the four-peaked EIA structure (2007, background): “…time (or Sun-synchronous) perspective, the E3 diurnal nonmigrating tide exhibits four lower thermospheric or E region maxima [e.g., Oberheide et al., 2003; Forbes et al., 2006] at the same longitude locations of the four strong equatorial ionization anomaly (EIA) zones [e.g., Immel et al., 2006].”
• Tidal propagation of deep tropical cloud signatures into the thermosphere from TIMED observations (2008, background): “Derived parameters are monthly mean tidal component amplitudes and phases in temperature T [Forbes et al., 2006; Zhang et al., 2006], and zonal and meridional winds (u, v) [Oberheide et al., 2006, 2007; Wu et al., 2006].”
• Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects (2009, unknown): “0148-0227/09/2009JD012388$09.00 D00I05 1 of 18 and a temporal coverage (7 years so far, 2002–2008) that was not possible before [Forbes et al., 2006, 2008; Zhang et al., 2006].”
• Implications for atmospheric dynamics derived from global observations of gravity wave momentum flux in stratosphere and mesosphere (2011, background): “In addition, the two strongest tidal components present in the stratosphere and mesosphere [e.g., Forbes et al., 2006; Mukhtarov et al., 2009; Pancheva et al., 2010] are accounted for: the diurnal westward tide with zonal wavenumber one (shortly called DW1 tide), as well as the diurnal eastward…”
• Assessment of the quality of the Version 1.07 temperature‐versus‐pressure profiles of the middle atmosphere from TIMED/SABER (2008, background): “Such large wave amplitudes may be associated with the localized breaking of gravity waves or due to interactions between the migrating tides and stationary planetary waves [Forbes et al., 2006].”