Migrating and nonmigrating semidiurnal tides in the upper atmosphere excited by tropospheric latent heat release: MIGRATING AND NONMIGRATING SEMIDIURNAL TIDES

By M. E. Hagan, Jeff Forbes. 2003

497 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/da8527a187fa6109b4e73d8e6192ea9c913ecc53

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

In Atmospheric Science

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

Citations in the corpus

• 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].”
• Troposphere-Thermosphere Tidal Coupling as Measured by the SABER Instrument on TIMED during July-September, 2002 (2006, methodology): “The dotted lines in Figure 3 correspond to the GSWM results (Hagan and Forbes, 2003).”
• Exploring earth's atmosphere with radio occultation: contributions to weather, climate and space weather (2011, unknown): “(Global-Scale Wave Model Version 2; Hagan and Forbes, 2002, 2003)”
• Solar tides as revealed by measurements of mesosphere temperature by the MLS experiment on UARS (2006, background): “…observational analyses spawned a number of modeling investigations seeking to explain the origins and characteristics of nonmigrating tides in the MLT (i.e., Ekanayake et al. 1997; Miyahara et al. 1999; Forbes et al. 2001; Hagan and Roble 2001; Grieger et al. 2002; Hagan and Forbes 2002, 2003).”
• Plausible effect of atmospheric tides on the equatorial ionosphere observed by the FORMOSAT‐3/COSMIC: Three‐dimensional electron density structures (2007, background): “…with a nonmigrating tide which is excited in the troposphere, possibly produced by the latent heat release in tropical cloud formation [e.g., Hagan and Forbes, 2002, 2003], propagating upward and subsequently affects the E-region dynamo electric field [Sagawa et al., 2005; Immel et al.,…”
• Longitudinal structure of the equatorial ionosphere: Time evolution of the four-peaked EIA structure (2007, methodology): “…Later, Immel et al. [2006] superimposed the global distribution of the nighttime equatorial anomaly peaks in the northern hemisphere observed by the IMAGE FUV and the E3 nonmigrating tide (represented in neutral temperature) simulated by the Global Scale Wave Model [Hagan and Forbes, 2002, 2003].”
• 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].”
• Seasonal variation of thermospheric density and composition (2009, methodology): “The TIE-GCM includes tidal effects using the GSWM [Hagan and Forbes, 2002, 2003].”
• Control of equatorial ionospheric morphology by atmospheric tides (2006, methodology): “[7] Overlaid on this image are contours of the equinoctial amplitude of the diurnal temperature variation at 115 km determined from the Global Scale Wave Model (GSWM) [Hagan et al., 2001; Hagan and Forbes, 2002, 2003; Forbes et al., 2003].”
• Connections between deep tropical clouds and the Earth's ionosphere (2007, background): “However, only a subset of these waves propagates upward into the MLT, including the migrating components and the DE3 [Hagan and Forbes, 2002, 2003].”
• Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects (2009, background): “[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].”