Dipole Measurements of Waves in the Ionosphere
Dipole Measurements of Waves in the Ionosphere
复制标题
电离层波的偶极子测量
DOI:
10.1007/3-540-33203-0_7
复制
发表时间:
2006
期刊:
影响因子:
--
通讯作者:
H. G. James
中科院分区:
文献类型:
--
作者:
H. G. James
AbstractThe theory of distributed dipole antennas in magnetoplasmas has been tested through the analysis of the data from the two-point propagation experiment OEDIPUS C (OC). The transmission of electromagnetic signals over a 1-km distance in the ionosphere has been used to substantiate the theory of emission, propagation and detection of waves in a cold magnetoplasma. Confirmations and insights about the dipole theory arising from the OC research results have occasioned a return to some older data that can be profitably interpreted with them. The concept of dipole effective lengthLeffhas been re-examined quantitatively with the help of the reciprocity principle. It is found that previous measurements of electromagnetic whistler-mode propagation giveLeffvalues similar to those predicted using a classic reciprocity definition brought over from the vacuum dipole theory. In contrast, OC investigations found thatLeffcan be many times the dipole physical length for propagation near the whistler-mode resonance cone. The finding has important consequences for the interpretation of the measured strength of the radio emission auroral hiss and, by extension, the nature of its source. Since intra-ionospheric experiments on propagation near either the lower- or the upper-oblique-resonance cone produced extremely strong transmission, theLeffapplied to the interpretation of the strength of plasma-wave phenomena in the corresponding frequency domains must be chosen with care.