The DOI matches its Crossref record; 22 of the 22 references it cites were found in a registry or an index.
Linear theory and modeling of the Rayleigh‐Taylor instability leading to the occurrence of equatorial spread F
Abstract
In a test of the generally accepted Rayleigh‐Taylor (R‐T) instability mechanism for equatorial spread F (ESF), a linear instability growth rate γRT is derived following the formalism of Haerendel (preprint, 1973) which takes into account the variations of physical parameters along geomagnetic flux tubes. The resulting form of γRT extends the results of previous work by including direct dependencies on transequatorial neutral winds, zonal electric fields, vertical and horizontal ionospheric density gradients, the presence of an E region, and chemical recombination. Realistic atmospheric and ionospheric density model inputs are used for the first time to make quantitative calculations of R‐T growth rates for a range of geophysical conditions. The key result of this study is that time/altitude domains having positive calculated instability growth rates are found to coincide with observed time/altitude patterns of ESF occurrence over both a monthly and a yearly time frame. This success in being able to model the climatological occurrence of ESF lends support to the physical model adopted for the instability mechanism and opens up new avenues of research into ESF predictability on a night‐to‐night and even an hour‐to‐hour basis.
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Cites
Hedin, A. E. (1987) · Journal of Geophysical Research: Space Physics · doi:10.1029/ja092ia05p04649 · Cited by 1,720
The Earth's Ionosphere - Plasma Physics and Electrodynamics
(1989) · International Geophysics · doi:10.1016/s0074-6142(09)x6010-9 · Cited by 1,089
Radar observations of F region equatorial irregularities
Woodman, R. F., & La Hoz, C. (1976) · Journal of Geophysical Research · doi:10.1029/ja081i031p05447 · Cited by 1,059
Kelley, M. C. (1989) · Cited by 781
Revised global model of thermosphere winds using satellite and ground‐based observations
Hedin, A. E., Biondi, M. A., Burnside, R. G., Hernandez, G., Johnson, R. M., Killeen, T. L., Amory‐Mazaudier, C., Meriwether, J. W., Salah, J. E., Sica, R. J., et al. (1991) · Journal of Geophysical Research Atmospheres · doi:10.1029/91ja00251 · Cited by 636
Tsunoda, R. T. (1985) · Journal of Geophysical Research: Space Physics · doi:10.1029/ja090ia01p00447 · Cited by 522
Equatorial spread F: Implications of VHF radar observations
Farley, D. T., Balsey, B. B., Woodman, R. F., & McClure, J. P. (1970) · Journal of Geophysical Research · doi:10.1029/ja075i034p07199 · Cited by 463
Nonlinear equatorial spread F: The effect of neutral winds and background Pedersen conductivity
Zalesak, S. T., Ossakow, S. L., & Chaturvedi, P. K. (1982) · Journal of Geophysical Research: Space Physics · doi:10.1029/ja087ia01p00151 · Cited by 348
The longitudinal morphology of equatorial F-layer irregularities relevant to their occurrence
Aarons, J. (1993) · Space Science Reviews · doi:10.1007/bf00750769 · Cited by 309
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Cited by
Basu, S., Groves, K. M., Basu, S., & Sultan, P. J. (2002) · Journal of Atmospheric and Solar-Terrestrial Physics · doi:10.1016/s1364-6826(02)00124-4 · Cited by 328
Self-citationLongitudinal variability of equatorial plasma bubbles observed by DMSP and ROCSAT‐1
Burke, W. J., Gentile, L. C., Huang, C. Y., Valladares, C. E., & Su, S. Y. (2004) · Journal of Geophysical Research: Space Physics · doi:10.1029/2004ja010583 · Cited by 317
Metadata
- Authors
- Sultan, P. J.
- Venue
- Journal of Geophysical Research: Space Physics
- Publisher
- American Geophysical Union (AGU)
- Published
- 1996-12
- Volume
- 101
- Issue
- A12
- Pages
- 26875-26891
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W1991378411
- Cited by
- 621
- References
- 22
- FWCI
- 3.63
- Type
- journal article
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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