Aerodynamical Mechanisms Producing Electronic Density Fluctuations in Turbulent Ionized Layers
- 1 January 1955
- journal article
- Published by Institute of Electrical and Electronics Engineers (IEEE) in Proceedings of the IRE
- Vol. 43 (10), 1240-1252
- https://doi.org/10.1109/jrproc.1955.277936
Abstract
Various radio effects of the turbulence in the low ionosphere are discussed with a view toward determining the order of magnitude of the turbulence parameters in this region. These effects include vhf scattering, sporadic E-layer phenomena, and diffraction patterns in reflection. The required electron density fluctuations (ΔN/N)2 fluctuate around 10-4 and the scale of the turbulence I is roughly 100 to 200 meters. The latter quantity measured directly in the troposphere is of about the same order of magnitude. The underlying purpose of the paper is to study the aerodynamical mechanisms of turbulence. Pressure fluctuations result from the "collisions and extensions between turbulent eddies" in a uniform gas, or from vertical transport in the atmosphere with its varying pressure. It is shown that such pressure fluctuations are too small, by a factor of about 10-4, to produce the observed density fluctuations. However, the vertical transport mechanism produces two other effects which are independent of the energy of the turbulence and are of the right order of intensity. First, in a nonadiabatic atmosphere the vertical transport of air masses produces fluctuations of temperature. These, in turn, give rise to air density fluctuations, and proportional electron density fluctuations. Second, fluctuations of electron density result directly from transport in the presence of a gradient of electron density. These two effects, for the same uniform turbulence, occur at different levels in an ionospheric layer. They are sufficient to explain the stratification properties of sporadic E.Keywords
This publication has 18 references indexed in Scilit:
- Movement of theF-regionJournal of Geophysical Research, 1955
- Radio Transmission at VHF by Scattering and Other Processes in the Lower IonosphereProceedings of the IRE, 1955
- Winds at altitudes up to 80 kilometersJournal of Geophysical Research, 1954
- The Scattering of Electromagnetic Waves by Turbulent Atmospheric FluctuationsPhysical Review B, 1954
- Measurements of winds in the upper atmosphere by means of drifting meteor trails IIJournal of Atmospheric and Terrestrial Physics, 1953
- A statistical survey of atmospheric index-of-refraction variationTransactions of the IRE Professional Group on Antennas and Propagation, 1953
- A New Kind of Radio Propagation at Very High Frequencies Observable over Long DistancesPhysical Review B, 1952
- A radio echo method for the investigation of atmospheric winds at altitudes of 80 to 100 kmJournal of Atmospheric and Terrestrial Physics, 1952
- A Study of the Horizontal Irregularities of the IonosphereProceedings of the Physical Society. Section B, 1950
- Diffraction from an irregular screen with applications to ionospheric problemsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1950