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1.
We present the results of studies of the multifractal structure of slow (of duration τ ≈ 10 s) fluctuations of the received-signal
amplitudes in special experiments on radio-raying of the midlatitude ionosphere by signals from orbital satellites in 2004–2006.
It is shown, in particular, that the method of multifractal analysis of amplitude records of the received signals yields information
on the spectrum of large-scale ionospheric inhomogeneities, which is inaccessible for the classical method of radio scintillations.
From the results of measurements with the use of multifractal processing of experimental data, we found that large-scale (tens
of kilometers) quasiregular electron-density inhomogeneities of traveling ionospheric disturbances (TIDs) have a power-law
spectrum. It is exactly the power-law form of the spatial spectrum of large-scale inhomogeneities of TIDs that can be the
reason for the observed multifractal structure of the intermittency of slow fluctuations of the received-signal amplitudes.
However, under conditions of a developed small-scale turbulence of TIDs, the observed multifractal structure of the received
signals is, as a rule, stipulated by the spatial inhomogeneity of the variance of the integral electron-density fluctuations
of small-scale inhomogeneities on scales comparable with the sizes of large-scale inhomogeneities of TIDs.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 3, pp. 191–198, March 2008. 相似文献
2.
We present the results of the studies of fractal properties of the small-scale inhomogeneities of traveling ionospheric disturbances
in special experiments on radio-raying of the midlatitude ionosphere by signals from orbital satellites in 2004–2006. Along
with the conventional correlation processing of the received signals, we performed their multifractal analysis, as well as
fractal processing of signals by the correlation-integral method. Important information on fractal properties of the small-scale
turbulence for the least studied part of the upper-ionosphere inhomogeneity spectrum in the interval of characteristic scales
l ≈ 1–10 km is obtained. In particular, it is noted that the fractal structure of these inhomogeneities can be originated
from the nonlinear “destruction” of several large-scale sinusoidal structures in a quasistable traveling disturbance. It is
also noted that the multifractal spectra of amplitude fluctuations of the received signals obtained in the experiments in
different years, in different time of the day, and in different seasons of the observations are quite similar. This is evidence
that intermittency is a universal property of the plasma turbulence, at least for the midlatitude upper ionosphere.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 1, pp. 22–30, January 2008. 相似文献
3.
We present the results of the first studies of the fractal structure of the developed small-scale ionospheric turbulence (SSIT)
during special experiments on radio-raying of the midlatitude ionosphere by signals from orbital satellites in 2005–2006.
It is established that under conditions of developed turbulence, typical values of the fractal dimension of the space occupied
by natural SSIT inhomogeneities are, as a rule, close to the topological dimension of their embedding space, and the true
values of the spectral index of isotropic SSIT only slightly differ from the corresponding generally accepted nominal values
in the embedding space. Nevertheless, even small differences in the mentioned parameters detected in the experiment witness
a sharply nonuniform distribution of the local fractal structures of the developed SSIT in space. We propose a stochastic
model of the nonstationary process for fast amplitude fluctuations of signals during their propagation in the ionosphere with
nonuniform spatial distribution of small-scale electron-density fluctuations. Eventually, namely this nonuniform distribution
of small-scale electron-density fluctuations leads to the specific multifractal structure of the amplitude records of received
signals.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 4, pp. 287–294, April 2008. 相似文献
4.
We consider the problem of relating the local structure of small-scale ionospheric turbulence to the measured frequency-spectrum
indices and fractal dimensions of amplitude records of the signals received on the Earth during remote sensing of the ionosphere
onboard the satellites. It is shown that knowledge of these parameters permits one to determine the true values of the local-spectrum
indices of the electron-density fluctuations for isotropic small-scale turbulence of the ionosphere both under natural conditions
and during its modification by high-power short-wave radiation as well as to specify fractal dimensions of space filled by
small-scale irregularities of the turbulent structures in the ionosphere. We show the necessity of detailed experimental studies
of the fractal properties of small-scale ionospheric irregularities of both natural and artificial origin by using a multifractal
analysis in combination with the synchronous correlation processing of received signals during remote sensing of the ionosphere.
This will give important information on the local structure of small-scale ionospheric turbulence inaccessible for studies
within the framework of the classical method of radio scintillation.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 50, No. 4, pp. 300–308, April 2007. 相似文献
5.
V. A. Alimov F. I. Vybornov L. M. Erukhimov G. P. Komrakov N. A. Mityakov A. V. Rakhlin 《Radiophysics and Quantum Electronics》1997,40(6):456-458
We show some results of experiments on synchronous sounding of the ionosphere by short-wave signals at the Radiophysical Research
Institute’s test site in Zimenki and Vasil’sursk, Nizhniy Novgorod province, during ionospheric modification by high-power
short radiowaves from transmitters of the “Sura” facility in Vasil’sursk. In the course of experiments we proved directly
the decisive role of large-scale inhomogeneities of the ionospheric plasma with dimensions of from several kilometers to several
dozens of kilometers in the formation of artificial F- spread. The small-scale inhomogeneities with dimensions smaller than
1 km, which are localized in a relatively thin layer near the reflection level of a high-power short radiowave, emerged only
at sounding waves, propagating (reflected) in the immediate vicinity of the center of the heating region.
Radiophysical Research Institute, Nizhny Novgorod, Russia. Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika,
Vol. 40, No. 6, pp. 688–692, June, 1997. 相似文献
6.
N. V. Bakhmet'eva V. V. Belikovich L. M. Kagan A. A. Ponyatov A. V. Tolmacheva M. C. Kelley M. J. Nicolls 《Radiophysics and Quantum Electronics》2005,48(9):673-685
We present the results of studying the lower ionosphere in 2000–2004 at the “Sura” heating facility by the method of resonance
scattering of radio waves from artificial periodic inhomogeneities of the ionospheric plasma. Experimental data on a study
of the sunset–sunrise phenomena in the ionospheric D region and the possibility of determining the concentrations of atomic
oxygen and excited molecular oxygen are discussed. The results of studying the sporadic layers of ionization are presented
and the method for a study of ion composition of the Es layer is discussed. Data of the August 2004 experiments on a study of the influence of heating the ionosphere on the Es layer and characteristics of artificial periodic inhomogeneities are presented. Prospects for further research are discussed.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 48, No. 9, pp. 757–771, September 2005. 相似文献
7.
V. A. Alimov F. I.Vybornov E. N. Myasnikov A. V. Rakhlin V. L. Frolov 《Radiophysics and Quantum Electronics》2009,52(9):609-617
We present the results of the experiment on studying the multifractal structure (with inhomogeneity sizes from tens to hundreds
of meters across the Earth’s magnetic field) of the artificial ionospheric turbulence when the midlatitude ionosphere is affected
by high-power HF radio waves. The experimental studies were performed on the basis of the “Sura” heating facility with the
help of radio sounding of the disturbed region of the ionospheric plasma by signals from the Earth’s orbital satellites. The
influence of the magnetic zenith effect on measured multifractal characteristics of the small-scale artificial turbulence
of the midlatitude ionosphere was examined. In the case of vertical radio sounding of the disturbed ionosphere region, the
measured multipower and generalized multifractal spectra of turbulence coincide well with similar multifractal characteristics
of the ionospheric turbulence under natural conditions. This result is explained by the fact that the scattering of signals
by weak quasi-isotropic small-scale inhomogeneities of the electron number density in a thick layer with a typical size of
several hundred kilometers above the region of reflection of high-power HF radio waves gives the major contribution to the
observed amplitude fluctuations of received signals. In the case of oblique sounding of the disturbance region at small angles
between the line of sight to the satellite and the direction of the Earth’s magnetic field, the nonuniform structure of the
small-scale turbulence with a relatively narrow multipower spectrum and small variations in the generalized multifractal spectrum
of the electron number density was detected. Such a fairly well ordered structure of the turbulence is explained by the influence
of the magnetic zenith effect on the generation of anisotropic small-scale artificial turbulence in a thin layer having a
typical size of several ten kilometers and located below the pump-wave reflection height in the upper ionosphere. 相似文献
8.
We report on the results of studying the lower ionosphere by a method based on the resonant scattering of radio waves by artificial
periodic inhomogeneities of the ionospheric plasma. Different aspects of studying the sporadic E layer such as the influence of the vertical transfer on its formation, the possibility of examination of its ion composition,
and the influence of the ionosphere heating on the layer characteristics are discussed. The results of determining the parameters
of the E
s layer and some characteristics of the lower ionosphere during the creation of artificial periodic inhomogeneities at two
frequencies are presented.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 11, pp. 956–969, November 2008. 相似文献
9.
We present the results of new studies of the sporadic E layer in the case of heating of the ionosphere by high-power HF radio
emission. The measurements were performed at the “Sura” heating facility. Ionosphere was modified by high-power radio emission
from the “Sura” facility and was sounded by the probing radio waves of the same frequency and mode. The heating of the ionosphere
resulted in the formation of artificial periodic inhomogeneities, and an increase in the intensity of all signals scattered
by the D, E, and F regions and the sporadic E layer by 5–20 dB was observed. The increase was observed during heating of the
ionosphere by each magnetoionic component, but was smaller for heating by an ordinary-mode wave. This effect was resonant
and disappeared as a result of the frequency detuning down to 85 kHz. During the ionospheric modification, the signal-intensity
increased due to modulation of the natural profile of the electron number density by the artificial periodic structure.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 50, No. 8, pp. 695–708, August 2007. 相似文献
10.
We analyze the propagation of wave perturbations of plasma density in the outermost part of the ionospheric F-region. It is
shown that growing oscillations can propagate downwards along the geomagnetic field lines. Such perturbations can form random
inhomogeneities in the upper ionosphere.
State University, Irkutsk, Russia. Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 41, No. 4, pp.
432–437, April, 1998. 相似文献
11.
Bakhmet'eva N. V. Belikovich V. V. Benediktov E. A. 《Radiophysics and Quantum Electronics》2001,44(12):924-934
We present new results of our studies of the irregular structure of the ionosphere using artificial periodic inhomogeneities (APIs) of the ionospheric plasma. The observations were carried out from 9:00 to 17:00 in August 10–12, 1999 with a height step of 0.7 km and digital registration and real-time processing of the signal quadratures. It is shown that in many cases, the amplitude of the scattered signal is determined by the interference of radio waves scattered on APIs and on natural ionospheric formations including sporadic layers and large-scale natural irregularities. This allows one to study the irregular structure of the lower ionosphere by analyzing height-time dependences of the amplitude and phase of the scattered signal. 相似文献
12.
V. P. Uryadov G. G. Vertogradov V. G. Vertogradov S. V. Kubatko A. A. Ponyatov Yu. N. Cherkashin I. V. Krasheninnikov V. A. Valov G. P. Komrakov A. V. Makarov D. V. Bredikhin 《Radiophysics and Quantum Electronics》2009,52(4):241-251
We describe the operation of an ionosonde/position finder with chirp modulation of the signal. The first results of measuring
the characteristics of short-wave radio signals scattered by artificial small-scale inhomogeneities, which were obtained by
means of an ionosonde/position finder on the IZMIRAN—“SURA”—Rostov-on-Don path are presented. It was found that under certain
ionospheric conditions, the angular and frequency selection of the scattered signals take place, in which case the signals
are observed simultaneously in several frequency intervals (mainly, in three, namely, 6–9.5 MHz, 10–12 MHz, and 15–18 MHz)
with different angles of incidence of radio waves in the vertical plane. In this case, the incidence angles were 20◦–35◦,
18◦–32◦, and 10◦–20◦ from the horizon for the first, second, and third frequency interval, respectively. Ionograms of oblique
sounding were modeled allowing for the scattering of radio waves by artificial small-scale inhomogeneities. It is shown that
at frequencies from 10 to 12 MHz, aspect conditions are fulfilled for the signals ducting along the high-angle beam (Pedersen
mode). At frequencies 15–18 MHz (higher than the maximum observable frequency of the forward signal on the path IZMIRAN—Rostov-on-Don),
aspect scattering conditions are fulfilled for the signals incident on a scattering area in the ascending part of the trajectory.
At low frequencies 6–9.5 MHz (below the maximum observed frequency of the forward signal on the IZMIRAN—Rostov-on-Don path),
the observable additional signals are caused by the scattering of radio waves by artificial inhomogeneities with subsequent
relfection of the scattered signal from the Earth on the “SURA”—Rostov-on-Don path.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 52, No. 4, pp. 267–278, April 2009. 相似文献
13.
G. N. Boiko S. M. Grach E. N. Sergeev G. P. Komrakov N. A. Mityakov K. Groves 《Radiophysics and Quantum Electronics》1999,42(7):601-608
On October 24, 1997, from 16:00 to 19:30 LT, during experiments on the artificial mofification of ionosphere by powerful HF
radiation using spaced heating, we recorded twice a significant (tens of percent) decrease of the electron number density
in the F-layer, synchronous with the operation of the heating trnasmitters. The critical frequency of this layer decreased
by 10–20%. This points to the possibility of artificial generation of large-scale inhomogeneities of the ionospheric plasma
density using spatially split heating.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 42, No. 7, pp. 682–690, January 1999. 相似文献
14.
We consider the problem of diagnostics of the local structure of small-scale ionospheric turbulence using the multifractal
analysis of received signals from the Earth’s orbital satellites after the radio sounding of the inhomogeneous ionosphere
by these signals. In particular, it is shown that analysis of the multifractal structure of the received-signal amplitude
records by the method of multidimensional structural functions allows one to determine the indices of the multipower local
spectra of the small-scale ionospheric turbulence, which are inherent in it due to the nonuniform spatial distribution of
small-scale fluctuations of the electron number density. It is noted that information on the multipower spectrum of small-scale
ionospheric turbulence is not available for the conventional radio scintillation method based on the classical spectral analysis
of received signals during the remote radio sounding of the ionosphere. At the same time, the method of multidimensional structural
functions is efficient under conditions of actual nonstationarity of the process of scattering of the HF radio waves by the
randomly inhomogeneous ionospheric plasma. The method of multidimensional structural functions is used for the multifractal
processing of received signals of orbital satellites during special experiments on radio sounding of the midlatitude ionosphere
under natural conditions and its modification by high-power HF radio waves. First data on the indices of the multipower local
spectra of small-scale ionospheric turbulence are obtained.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 52, No. 1, pp. 14–22, January 2009. 相似文献
15.
V. A. Alimov F. I. Vybornov E. N. Myasnikov A. V. Rakhlin 《Radiophysics and Quantum Electronics》2008,51(11):874-879
We show the results of the first experimental studies of the multifractal structure of the developed artificial ionospheric
turbulence. As a result of the special multifractal analysis of the recorded amplitudes of signals from the orbital satellites,
which were obtained during the experiments on radio tomography of the irregularities excited in the ionosphere by the powerful
mid-latitude heating facility “Sura,” it is found that the characteristic multifractal structure of these records is caused
by the nonuniform spatial distribution of the small-scale fluctuations of the electron number density in the artificial irregularities
of the ionospheric plasma. Comparative analysis is performed for the multifractal spectra of fluctuations of both the amplitudes
and energies of signals received from the orbital satellites upon radio transmission probing of the region of artificial ionospheric
turbulence by these signals at three observation points located near the “Sura” heating facility and spaced apart to a distance
of about 100–150 km.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 11, pp. 970–976, November 2008. 相似文献
16.
We present the results of studying the multifractal structure of intermittency in a developed ionospheric turbulence during
special experiments on radio-raying of the midlatitude ionosphere by signals from orbital satellites in 2005–2006. It is shown,
in particular, that the determination of multidimensional structural functions of the energy fluctuations of received signals
permits one to obtain the necessary information on multifractal spectra of the studied process of radio-wave scattering in
the ionosphere. Experimental data on multifractal spectra of slow fluctuations in the received-signal energy under conditions
of a developed small-scale turbulence are compared with the existing concept of the radio-wave scattering within the framework
of the statistical theory of radio-wave propagation in the ionosphere. It is inferred that under conditions of a developed
ionospheric turbulence, the multifractal structure of the intermittency of slow fluctuations in the received-signal energy
is a consequence of the intermittency of small-scale fluctuations in the electron number density of the ionospheric plasma
on relatively large spatial scales of about several ten kilometers.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 6, pp. 485–493, June 2008. 相似文献
17.
We consider the problem of obtaining reliable values of the local-spectrum indices of the electron number density fluctuations
for small-scale ionospheric turbulence. It is shown that the use of a multifractal analysis in combination with the synchronous
correlation processing of the received signals in the experiments on remote radio sounding of the ionosphere by satellite
signals permits one to solve the posed problem. In this case, the true values of the local-spectrum indices of small-scale
ionospheric turbulence, which are measured in such specialized experiments under natural conditions and during modification
of the ionosphere by high-power HF radio emission, can differ notably from their standard values obtained within the framework
of the classical method of radio scintillations, in which only correlation processing of the data is used.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 7, pp. 571–574, July 2008. 相似文献
18.
We report on the results of observations of reflected SW signals by vertical sounding (VS) of the ionosphere in Zimenki, Nizhny Novgorod region, in the summers of 1994 and 1995. We discovered an anomalous increase in the multipath propagation of the received SW signals during ionospheric F-spread: The duration of a multipath reflected signal increased considerably when we used a highly directional antenna compared to the case of a weakly directional antenna. The fast amplitude fluctuation index increased with increasing delay of the reflected SW signals. The observations are interpreted in terms of a stochastic model of midlatitude F-spread as the phenomenon of multipath radio wave scattering (reflection) from large-scale electron density inhomogeneities under conditions of a strongly developed inhomogeneous structure of the ionosphere.Radiophysical Research Institute, Nizhny Novgorod. Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 38, No. 10, pp. 1064–1070, October, 1995. 相似文献
19.
V. V. Belikovich N. V. Bakhmeteva E. E. Kalinina A. V. Tolmacheva 《Radiophysics and Quantum Electronics》2006,49(9):669-674
We propose a new method for determination of the electron number density in the E region of the ionosphere on the basis of
scattering of radio waves from artificial periodic inhomogeneities formed by the high-power radio emission at two frequencies
and having different spatial periods. The ratio of relaxation times of the artificial periodic inhomogeneities at a given
altitude is determined only by the ratio of their spatial periods, which makes it possible to determine electron number density.
The paper presents the corresponding calculations and the estimates of possible measurement errors.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 49, No. 9, pp. 744–750, September 2006. 相似文献
20.
E. D. Tereshchenko A. N. Milichenko V. L. Frolov R. Yu. Yurik 《Radiophysics and Quantum Electronics》2008,51(11):842-846
We present the results of first studies of the modification of the ionosphere by high-power HF radiation, which were obtained
using signals of high-orbit GPS/GLONASS navigation satellites. Enhancement of the ionospheric modification in the magnetic-field
direction was observed for the first time. This leads to a total decrease in electron number density and the formation of
electron density irregularities near the magnetic-zenith direction. The efficiency of using GSP/GLONASS satellite signals
for the studies of the ionosphere modified by HF radiation is demonstrated. Prospects for further studies in this field are
discussed.
Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 51, No. 11, pp. 934–938, November 2008. 相似文献