Titlebook: Low-Frequency Waves and Irregularities in the Ionosphere; Proceedings of the 2 N. D’angelo Conference proceedings 1969 Springer Science+Bus

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JADED

Effects of Ion-Atom Collisions on the Propagation and Damping of Ion-Acoustic Waves,/.. from 1 to approximately 3–4, caused by ion-atom collisions, results in a decrease of the (Landau) damping of the waves. At high gas pressure and/or low wave frequency a ‘fluid’ picture adequately describes the experimental results.

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Canvas

使苦惱

Role of the Universal Instability in Auroral Phenomena,at .. ≈ 6 may modulate particle precipitation into the ionospheric auroral regions and account for some of the observations on pulsating (optical) auroras and X-ray pulsations. It is shown that a good correlation exists between the temporal and spatial variations of particles precipitation and the p

勛章

Whistlers-Use for Determination of Composition and Temperature,spheric electron concentration from nose whistlers and the results concerning the ‘knee’ in the density profile and the plasmapause are discussed. From ion cyclotron whistlers the ion concentration, the electron concentration, the ion gyro-frequencies, and the ion temperatures in the ionosphere can

來就得意

Observations of Ionospheric Very-Low-Frequency Radio Noise,Island, Virginia, on 21 September 1967. The electric dipole and magnetic loop antenna systems and the VLF (30 Hz–70 kHz) receivers are described. Data on the spectral characteristics, the noise amplitude, and the wave field geometry for two types of noise are summarized. A high frequency electromagn

積極詞匯

VLF and LF Emissions at Auroral Latitudes,on. There are different types of noise classified according to their shape in a frequency—time spectrogram (Gallet, 1959), but they can all be characterized as either discrete noise, which has a clear structure in the spectrogram, or hiss, which has no or very little structure and so resembles white

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