Evidence for a Rayleigh‐Taylor type instability and upwelling of depleted density regions during equatorial spread F
- 1 August 1976
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 3 (8) , 448-450
- https://doi.org/10.1029/gl003i008p00448
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Calculations of equatorial scintillations at VHF and gigahertz frequencies based on a new model of the disturbed equatorial ionosphereGeophysical Research Letters, 1976
- Linear theory of equatorial spreadFJournal of Geophysical Research, 1975
- Steady state finite amplitude Rayleigh Taylor modes in spread FGeophysical Research Letters, 1975
- In situ measurements of the spectral characteristics ofFregion ionospheric irregularitiesJournal of Geophysical Research, 1974
- Equatorial spreadF: Recent observations and a new interpretationJournal of Geophysical Research, 1972
- A satellite survey of vector electric fields in the ionosphere at frequencies of 10 to 500 hertz: 3. Low-frequency equatorial emissions and their relationship to ionospheric turbulenceJournal of Geophysical Research, 1972
- Soft particle fluxes near the equatorJournal of Geophysical Research, 1971
- Equatorial spreadF: Implications of VHF radar observationsJournal of Geophysical Research, 1970
- Artificial strontium and barium clouds in the upper atmospherePlanetary and Space Science, 1967
- Convective diffusion in the equatorial F regionJournal of Atmospheric and Terrestrial Physics, 1956