Abstract:We present new results of studying the artificial periodic irregularities produced in the ionosphere by the radio emission of the high-power heating facility "Sura" during the period of observations of the sporadic E layer. Basing on the measurement results for the velocity of the vertical plasma motion and the electron profile density in the E region of the ionosphere, which were obtained by the method of resonance scattering of radiowaves by an artificially produced periodic structure, we analyze the possibi… Show more
“…[] reported that decay times varied from a few milliseconds at the upper height (up to 140 km) for the few second at the lowest (80–90 km). Numerous API observations in D and E regions at Sura show the decay time of the same order as at HAARP [ Bakhmetieva and Belikovich , 2008; Bakhmetieva et al , , ]. Usually, APIs in the D and E regions existed throughout all experiments at the midlatitudes and show high variability of the echo amplitude at all heights.…”
Section: Discussionmentioning
confidence: 80%
“…[, , ]. The most recent experiments on the API formation were carried out using similar pumping and probing waves [ Bakhmet ' eva et al ., , , ; Bakhmetieva and Belikovich , , ; Grigoriev et al ., ; Tolmacheva et al ., ].…”
Section: Api Techniquementioning
confidence: 99%
“…The maximum of amplitude of the API scattered signal corresponds to the height of the maximum of the E region. In the left plot of Figure prior API generation sporadic E layer is not available, but API technique allows to detect very weak sporadic layers [ Belikovich et al ., ; Kagan et al ., ; Bakhmet ' eva et al ., ].…”
Section: Api Observations At Haarpmentioning
confidence: 99%
“…[], Bakhmetieva and Belikovich [], and Bakhmet'eva et al . []. Effect of sporadic E layer on the APIs is manifested by the local growth of the signal amplitude by as high as 30–40 dB at the altitudes of E s layer.…”
Section: Api Observations At Haarpmentioning
confidence: 99%
“…It should be noted that using the API technique, we can detect sporadic layers in the lower ionosphere including very weak sporadic ionization layers with an electron density lower than 10 4 cm −3 , which cannot be recorded by a conventional ionosonde [ Kagan et al ., ; Bakhmetieva and Belikovich , , ; Bakhmet ' eva et al ., ].…”
We present results of the new observations of artificial periodic irregularities (APIs) in the ionosphere using the High Frequency Active Auroral Research Program (HAARP) heating facility carried out in late May and early June 2014.The objective of this work is to detect API using high‐latitude facility and analyze possible differences of the temporal and spatial variations of the API echoes in the high (HAARP) and middle (Sura) latitudes. Irregularities were created by the powerful wave of X mode and were sounded using the short probing pulses signals of X mode. API echoes were observed in the D, E, and F regions of the ionosphere. Amplitudes and characteristic times of the API echoes were measured. The API growth and decay times at HAARP (high latitudes) observed were similar to those at the Sura heating facility (midlatitudes).
“…[] reported that decay times varied from a few milliseconds at the upper height (up to 140 km) for the few second at the lowest (80–90 km). Numerous API observations in D and E regions at Sura show the decay time of the same order as at HAARP [ Bakhmetieva and Belikovich , 2008; Bakhmetieva et al , , ]. Usually, APIs in the D and E regions existed throughout all experiments at the midlatitudes and show high variability of the echo amplitude at all heights.…”
Section: Discussionmentioning
confidence: 80%
“…[, , ]. The most recent experiments on the API formation were carried out using similar pumping and probing waves [ Bakhmet ' eva et al ., , , ; Bakhmetieva and Belikovich , , ; Grigoriev et al ., ; Tolmacheva et al ., ].…”
Section: Api Techniquementioning
confidence: 99%
“…The maximum of amplitude of the API scattered signal corresponds to the height of the maximum of the E region. In the left plot of Figure prior API generation sporadic E layer is not available, but API technique allows to detect very weak sporadic layers [ Belikovich et al ., ; Kagan et al ., ; Bakhmet ' eva et al ., ].…”
Section: Api Observations At Haarpmentioning
confidence: 99%
“…[], Bakhmetieva and Belikovich [], and Bakhmet'eva et al . []. Effect of sporadic E layer on the APIs is manifested by the local growth of the signal amplitude by as high as 30–40 dB at the altitudes of E s layer.…”
Section: Api Observations At Haarpmentioning
confidence: 99%
“…It should be noted that using the API technique, we can detect sporadic layers in the lower ionosphere including very weak sporadic ionization layers with an electron density lower than 10 4 cm −3 , which cannot be recorded by a conventional ionosonde [ Kagan et al ., ; Bakhmetieva and Belikovich , , ; Bakhmet ' eva et al ., ].…”
We present results of the new observations of artificial periodic irregularities (APIs) in the ionosphere using the High Frequency Active Auroral Research Program (HAARP) heating facility carried out in late May and early June 2014.The objective of this work is to detect API using high‐latitude facility and analyze possible differences of the temporal and spatial variations of the API echoes in the high (HAARP) and middle (Sura) latitudes. Irregularities were created by the powerful wave of X mode and were sounded using the short probing pulses signals of X mode. API echoes were observed in the D, E, and F regions of the ionosphere. Amplitudes and characteristic times of the API echoes were measured. The API growth and decay times at HAARP (high latitudes) observed were similar to those at the Sura heating facility (midlatitudes).
We present the results of measuring characteristics of the ionosphere and neutral atmosphere by the method of resonant scattering of radio waves by artificial periodic irregularities of the ionospheric plasma in the altitude range 90-120 km. It is shown that the altitude-time variations of the measured characteristics are in many respects stipulated by the propagation of atmospheric waves. Hydrodynamic instabilities in the mesosphere -lower thermosphere are analyzed. Criteria of development of different-type instabilities are presented. Contribution of different processes to the dynamics of the medium is estimated on the basis of the measurement results.
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