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Nonlinear Rayleigh-Taylor instabilities, atmospheric gravity waves and equatorial spread F

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JA00762· OSTI ID:86373
; ;  [1]
  1. Cornell Univ., Ithaca, NY (United States)

Although it is generally accepted that equatorial spread F (ESF) is due to nonlinear evolution of the Rayleigh-Taylor instability, a number of important properties of the process remain unexplained. In particular, the authors investigate two as yet unexplained features of ESF: the common dominance of very large scale features ({ge} 20 km) and their large amplitude. Although associated for years with spread F the authors show here for the first time that atmospheric gravity waves can initiate the Rayleigh-Taylor instability. In agreement with other analytical theories and computer simulations they find that the initiated instability will be saturated by nonlinear coupling of unstable modes to damped modes if the amplitude of the seed gravity wave is small. However, if the amplitude of the seed gravity wave is large enough, the relative plasma density perturbations can reach 50% or more, implying essentially no saturation. The required initial amplitudes are not unreasonable. In the latter case, significant enhancements and depletions of the plasma density occur within several hundred seconds. The analysis presented demonstrates the possibility that large-scale spread F is triggered by gravity waves with the Rayleigh-Taylor instability as a source of amplification. In a separate calculation the authors also show that large-amplitude plasma perturbations can be produced by an explosive instability of the Rayleigh-Taylor modes. It is found that the condition for explosive growth of the Rayleigh-Taylor modes can be satisfied in the ionospheric F region. The authors propose that the explosive mode couplings of the Rayleigh-Taylor instability is a possible mechanism for production of large-amplitude bottomside sinusoidal structures. 47 refs., 1 fig.

Sponsoring Organization:
USDOE
OSTI ID:
86373
Journal Information:
Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: A9 Vol. 98; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English

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