Experimental studies of the ionospheric alfvén cavity using observations of electromagnetic noise background over the solar cycle of 1985 to 1995

Belyaev, P. P.; Polyakov, S. V.; Ermakova, E. N.; Isaev, S. V.

doi:10.1007/bf02676584

Cited by 14 publications

(12 citation statements)

References 2 publications

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“…They give estimates for variations of the local f parameter of the SRS, observed at "Hylaty" in 2001-2003, of approximately 0.4-0.8 Hz, depending on the hour, and the season (higher values in September, October than in August). This is in agreement with the results of other observations at middle latitudes (Belyaev et al, 1990(Belyaev et al, , 1997, especially the observations in Karimshino, at the site of similar L-shell: L 2 (Molchanov et al, 2004).…”

Section: Acquisition and Analysis Of Datasupporting

confidence: 93%

“…Odzimek (ao64@ion.le.ac.uk) there (Bösinger et al, 2004). The observations were continued at the Nizhny Novgorod observational station "Novaya Zhizn" (Belyaev et al, 1997) and more events were observed at "Borok" and "Mondy" (Pokhotelov et al, 2003), and Karimshino (Molchanov et al, 2004), Russia. Single observations of the SRS were also made at low and middle latitudes, and noted by Hickey et al (1996), Kułak et al (1999), and Odzimek (2004a).…”

Section: Have Been Discoveredmentioning

confidence: 99%

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An automatic method to determine the frequency scale of the ionospheric Alfvén resonator using data from Hylaty station, Poland

Odzimek

Kulak²,

Michalec

et al. 2006

Ann. Geophys.

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Abstract. ULF/ELF magnetic field data recorded at the "Hylaty" station in Poland (49 • 19' N, 22 • 56' E; L 2) are analysed to find the characteristics of spectral resonance structures (SRS) in the frequency range 1-5 Hz, related to the ionospheric Alfvén resonator (IAR). An automatic procedure is employed to SRS events observed at "Hylaty" during the nighttime in 2001-2003, to calculate the parameter which determines the separation between the harmonics of the resonator, termed the frequency scale. Diurnal and seasonal variations of the frequency scale within the range of 0.4-0.8 Hz have been found. The usefulness and disadvantages of this particular method of SRS analysis, and of other methods, are discussed.

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Section: Acquisition and Analysis Of Datasupporting

confidence: 93%

Section: Have Been Discoveredmentioning

confidence: 99%

An automatic method to determine the frequency scale of the ionospheric Alfvén resonator using data from Hylaty station, Poland

Odzimek

Kulak²,

Michalec

et al. 2006

Ann. Geophys.

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“…Daily, seasonal, and cyclic variations in the properties of the IAR (Belyaev et al 1997;Yahnin et al 2003) were examined. Their relation to various geomagnetic and geophysical processes (Guglielmi et al 2006;Potapov et al 2008;Dovbnya et al 2010Dovbnya et al , 2012 and to the state of the ionosphere (Yahnin et al 2003;Hebden et al 2005;Parent et al 2010;Potapov et al 2014) was studied.…”

Section: Introductionmentioning

confidence: 99%

Use of the International Reference Ionosphere 2012 model to calculate emission frequency scale of the ionospheric Alfvén resonator

Potapov

Polyushkina

Dovbnya

2015

J. Space Weather Space Clim.

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We apply the IRI-2012 version of the International Reference Ionosphere model to calculate the difference between frequencies of adjacent harmonics (frequency scale) of the ionospheric Alfvén resonator (IAR) emission. The calculated values are compared with the frequency scale data obtained from search-coil magnetometer measurements. To obtain satisfactory results, it appeared necessary to modify the IRI-2012 model by replacing the vertical profile of ionospheric parameters adopted in the standard model with the profile elongated along the magnetic field lines. Subsequent improvement was obtained through the model correction by using local f 0 F 2 measurements. Finally, our results showed strong correlation between estimated and measured values of frequency scale with the root-mean-square error of 0.14 Hz, or 15%.

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“…It is supposed that the mechanism of influence should be connected with the parametric or Schumann resonance. The first four harmonics of the Schumann resonance are known: 7.8 Hz ± 1.5 Hz, 14.5, 20, 26 Hz (±0.3 Hz) [1][2][3]. Two main mechanisms of the resonance reaction of the organism to a weak electromagnetic fields are well known.…”

Section: Introductionmentioning

confidence: 99%

Organic Analysis of Peridotite Rocks from the Ashadze and Logatchev Hydrothermal Sites

2011

Physical Chemistry

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The possibility of recording physical changes in aqueos solutions caused by a unique field generated by the Teslar chip (TC) inside a quartz wristwatch has been studied using holographic interferometry. We show that the refraction index of degassed pure distilled water and aqueous solutions of L-tyrosine and b-alanine affected by the TC does not change during the first 10 minutes of influence. In contrast, a 1% aqueous solution of plasma extracted from the blood of a patient with heart vascular disease changes the refractive index when affected by the TC. The characteristic time of reaction is about 10 2 seconds. Based on our prior research experience, we state that the response of the system studied to the TC's field is similar to that stipulated by the action of a constant magnetic field with the intensity of 1.1 × 10 −3 T. Nevertheless, our team have unambiguously proved that the TC generates the inerton field, which is associated with a substructure of the matter waves (and, therefore, it does not relate to the electromagnetic nature). We could unambiguously prove that the TC generates the inerton field.

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Experimental studies of the ionospheric alfvén cavity using observations of electromagnetic noise background over the solar cycle of 1985 to 1995

Cited by 14 publications

References 2 publications

An automatic method to determine the frequency scale of the ionospheric Alfvén resonator using data from Hylaty station, Poland

An automatic method to determine the frequency scale of the ionospheric Alfvén resonator using data from Hylaty station, Poland

Use of the International Reference Ionosphere 2012 model to calculate emission frequency scale of the ionospheric Alfvén resonator

Organic Analysis of Peridotite Rocks from the Ashadze and Logatchev Hydrothermal Sites

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