Migrating and nonmigrating diurnal tides in the middle and upper atmosphere excited by tropospheric latent heat release

By M. E. Hagan, Jeff Forbes. 2002

807 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/3e75b0962c49f03225894f8be017f3011ef80372

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In Astronomy and Astrophysics

1. R. Akmaev
2. Jeff Forbes
3. J. Oberheide
4. R. Roble
5. M. E. Hagan
6. Astrid Maute
7. Liying Qian
8. K. Häusler

In Atmospheric Science

1. Jeff Forbes
2. Liying Qian
3. R. Akmaev
4. S. Solomon
5. J. Oberheide
6. Dong L. Wu
7. Han-Li Liu
8. T. Immel

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): “The E3 diurnal nonmigrating tide, as predicted by the Global Scale Wave Model (GSWM) [Hagan and Forbes, 2002], is excited by latent heat release in the troposphere.”
• Longitudinal structure of the equatorial anomaly in the nighttime ionosphere observed by IMAGE/FUV (2005, methodology): “With recent progress in the MLT (mesosphere-lower-thermosphere) modeling research, it was demonstrated that the nonmigrating tide originated in the tropospheric latent heat release has a significant amplitude in the E layer [Forbes et al., 1997; Hagan and Forbes, 2002, 2003 ].”
• Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, background): “[2006b] further demonstrated a clear correspondence between the non-migrating diurnal tides [Hagan and Forbes, 2002] and the morphology of the post sunset EIA.”
• Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects (2009, methodology): “[2] It is now well accepted that latent heating due to deep convection in the tropical troposphere is a major source of nonmigrating tides [Hagan and Forbes, 2002, 2003].”
• Exploring earth's atmosphere with radio occultation: contributions to weather, climate and space weather (2011, neutral): “(Global-Scale Wave Model Version 2; Hagan and Forbes, 2002, 2003)”
• Internal wave coupling processes in Earth's atmosphere (2014, neutral): “Tidal variability can be inferred from satellite measurements of infrared brightness temperature (Hagan and Forbes, 2002).”
• Longitudinal variation of the E‐region electric fields caused by atmospheric tides (2006, methodology): “Section 3 will discuss the comparison of the EIA and EEJ data to one another and to results from the Global Scale Wave Model 2002 (GSWM) [Hagan and Forbes, 2002].”
• Longitudinal variability of low‐latitude total electron content: Tidal influences (2007, methodology): “[25] The Immel et al. [2006] study also reported a phase shift in the peak brightness of their nighttime UV observations of about 20 to the east when compared to the diurnal peak amplitudes of the temperature variation at 115 km as given by the Global Scale Wave Model (GSWM) [Hagan et al., 2001; Ha”
• Monthly tidal temperatures 20–120 km from TIMED/SABER (2006, background): “This is also true for D0 and DW2 [Hagan and Forbes, 2002; Forbes and Wu, 2006; Forbes et al., 2006].”
• Tropospheric tidal effects on the middle and upper atmosphere (2009, background): “These GSWM results [Hagan and Forbes, 2002, 2003] include tropospheric tidal responses excited by the absorption of infrared radia- JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, A01302, doi:10.1029/2008JA013637, 2009 1High Altitude Observatory, National Center for Atmospheric Research, Boulder,…”
• Tidal perturbations and variability in the mesopause region over Fort Collins, CO (41N, 105W): Continuous multi‐day temperature and wind lidar observations (2004, result): “The results are compared to the corresponding tidal prediction from Global Scale Wave Models [Hagan and Forbes, 2002].”
• Troposphere-Thermosphere Tidal Coupling as Measured by the SABER Instrument on TIMED during July-September, 2002 (2006, background): “Also shown are similar results from the Global Scale Wave Model (GSWM, Hagan and Forbes, 2002, 2003).”
• Modeling the effects of gravity wave momentum deposition on the general circulation above the turbopause (2009, methodology): “Therefore, we prescribe tidal oscillations at the lower boundary from the global scale wave model (GSWM-02) [ Hagan and Forbes, 2003 ].”
• Electrodynamics of the formation of ionospheric wave number 4 longitudinal structure (2008, background): “The ionospheric structure has been considered to have some relation to nonmigrating tides, which are generated by latent heat release in the troposphere and propagating upward [ Hagan and Forbes, 2002 ], especially to the eastward propagating zonal wave number 3 diurnal tide (DE3), which has a wave ”
• Variability of thermosphere and ionosphere responses to solar flares (2011, background): “…empirical models [Solomon and Qian, 2005]; auroral electron precipitation [Roble and Ridley, 1987] and ionospheric convection driven by the magnetosphere‐ionosphere current system [Heelis et al., 1982]; and the amplitudes and phases of tides from the lower atmosphere [Hagan and Forbes, 2002, 2003].”
• Connections between deep tropical clouds and the Earth's ionosphere (2007, methodology): “However, only a subset of these waves propagates upward into the MLT, including the migrating components and the DE3 [Hagan and Forbes, 2002, 2003].”
• Planetary waves in coupling the lower and upper atmosphere (2007, background): “It should be noted that MUAM does not include the tropospheric sources of nonmigrating tides (Forbes et al., 1997; Hagan and Forbes, 2002; Ward et al., 2005) and the observed amplitudes of nonmigrating tides and long-period tidal modulation can, in reality, be even stronger.”