1966
DOI: 10.1002/rds19661199
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Characteristics of Ionospheric Es Propagation and Calculation of Es Signal Strength

Abstract: This report begins by describing the distribution of reflection points in the ionospheric E propagation as observed in the Far East. The ionospheric attenuation of theE, signal is statistically treated as a function of a ratio of the frequency used to the critical frequency, foE,, at the path midpoint;and its distance dependence is compared with the so-called secant law. The attenuation of two-hop

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Cited by 11 publications
(5 citation statements)
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“…Across the whole series, good correspondence can be seen between the locations of the concentrations of great circle path midpoints and the nearby ionosonde ftEs values. Precise and detailed correspondence should not be expected, because the ftEs figures represent snapshots at the middle of each period, the intense Es clouds are likely to be small, and the derived reflection points can only be approximations because of the possibility of off-axis paths [42]. Nonetheless, the structure and evolution of the event can clearly be seen.…”
Section: Case Study Discussionmentioning
confidence: 99%
“…Across the whole series, good correspondence can be seen between the locations of the concentrations of great circle path midpoints and the nearby ionosonde ftEs values. Precise and detailed correspondence should not be expected, because the ftEs figures represent snapshots at the middle of each period, the intense Es clouds are likely to be small, and the derived reflection points can only be approximations because of the possibility of off-axis paths [42]. Nonetheless, the structure and evolution of the event can clearly be seen.…”
Section: Case Study Discussionmentioning
confidence: 99%
“…The mechanism for the oblique reflection of radio waves from Es layers is not well understood, with candidates including specular reflection [11], [12], [45], scattering [11], [12], and magneto-ionic double refraction [13]. Magneto-ionic double refraction in the ionosphere, whereby a wave launched vertically is split into two circularly polarized waves which travel at different speeds and, therefore, exhibit different time delays on reflection back to ground, was first observed in the 1930s [1].…”
Section: B Es Radio Wave Propagation Mechanismsmentioning
confidence: 99%
“…On that basis, but taking account of the fact that the antennas are of identical materials and construction (the principal sources of modeling errors), the characteristics of the two antennas are estimated to differ by less than 0.7 dB and 5 • . 6) Antenna off-axis bias: NEC-4 modeling indicates that signal deviations off-axis, due either to errors in antenna pointing or to Es reflection via indirect paths [45], could cause additional biases of up to 1 dB in gain and up to 2 • in phase for a 15 • azimuth deviation from the true direction to the beacon. 7) Ground reflection bias: due to Es reflection height uncertainty, a range of possible elevation angles must be considered.…”
Section: Measurement Uncertaintymentioning
confidence: 99%
“…Seasonal maps of probability of sporadic E occurrence at foEs >7 MHz for four regions (the Europe and Northern Africa, Northern America, Far East, and other regions) are calculated by Smith (1978). For estimation of probability of a radio communication through sporadic ELayer in VHF-band the Japanese researchers offered a set of curves of foEs distribution and a set of daily foEs variations, observed with various probability for various regions of globe: the Europe and Northern Africa (region A), Northern America (region B), and Far East (region C) (Miya and Sasaki, 1966). This technique subsequently after numerous improvements had been accepted by CCIR (1978CCIR ( -1990.…”
Section: Technique Of Modellingmentioning
confidence: 99%