2009
DOI: 10.5194/angeo-27-1657-2009
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The impact of gravity waves rising from convection in the lower atmosphere on the generation and nonlinear evolution of equatorial bubble

Abstract: Abstract. The nonlinear evolution of equatorial F-region plasma bubbles under varying ambient ionospheric conditions and gravity wave seeding perturbations in the bottomside F-layer is studied. To do so, the gravity wave propagation from the convective source region in the lower atmosphere to the thermosphere is simulated using a model of gravity wave propagation in a compressible atmosphere. The wind perturbation associated with this gravity wave is taken as a seeding perturbation in the bottomside F-region t… Show more

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Cited by 48 publications
(49 citation statements)
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“…Finally, the occurrence of topside ESF structures despite weak PRE peaks could also be associated with strong initial perturbations provided by atmospheric gravity waves as suggested by theoretical studies (e.g. Kherani et al, 2009). …”
Section: Day-to-day Variabilitymentioning
confidence: 88%
See 1 more Smart Citation
“…Finally, the occurrence of topside ESF structures despite weak PRE peaks could also be associated with strong initial perturbations provided by atmospheric gravity waves as suggested by theoretical studies (e.g. Kherani et al, 2009). …”
Section: Day-to-day Variabilitymentioning
confidence: 88%
“…Previous studies have also suggested that initial density perturbations (seed waves) could play a significant role in the development of ESF (e.g. Abdu et al, 2009;Kherani et al, 2009;Tsunoda, 2010). The low ESF occurrence despite a significant PRE could be attributed to the absence of triggering perturbations.…”
Section: Monthly Variabilitymentioning
confidence: 98%
“…To infer the development of EPB under the action of CII for simplified cases, we monitor the time history of the maximum vertical velocity (v max , the vertical component of ıE u ) inside the density depletion. The linear, exponential, and multiexponential growth of this velocity with time represent, respectively, the steady state, linear growth, and nonlinear growth (or the development of the EPB) of CII [Kherani et al, 2009].…”
Section: Simplified Prvd Configuration: Cases I-ivmentioning
confidence: 99%
“…These studies revealed the generation of the EPB initiated by a seed perturbation at the bottomside of the rising F layer. The seed perturbation used is either in the form of plasma density perturbation [Kherani et al, 2004;Huba and Joyce, 2007] or of wind perturbation [Huang and Kelley, 1996a;Kherani et al, 2009;Keskinen, 2010]. The seed perturbation may also arise from the shear instability as shown by Aveiro et al [2011].…”
Section: Introductionmentioning
confidence: 99%
“…The requirements on the PRE/evening vertical drift and the height of the F layer for the spread F "on" and "off" conditions and its varying growth rates and intensities have been widely discussed in the literature (e.g., Farley et al, 1970;Abdu et al, 1983Abdu et al, , 2006Fejer et al, 1999;Sultan, 1996;Sastri et al, 1997). Models have been developed to investigate the effects of the evening zonal electric fields, F layer bottom-side density gradients, and zonal, meridional and vertical winds on the ESF instability development conditions (e.g., Zalesak et al, 1982;Sekar et al, 1994;Maruyama, 1988;Keskinen et al, 2003;Kudeki et al, 2007;Kherani et al, 2009a). An important prerequisite concerns the nature and the intensity of the density perturbation needed to initiate the instability growth, which appears to be the least understood aspect of the ESF processes.…”
Section: Introductionmentioning
confidence: 99%