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Vitaly P. Kim,Valery V. Hegai 한국우주과학회 2015 Journal of Astronomy and Space Sciences Vol.32 No.2
In this paper we study the transmission of the electrostatic field due to coulomb charges of an individual thundercloud into the midlatitude ionosphere, taking into account the total geomagnetic field integrated Pedersen conductivity of the ionosphere. It is shown that at ionospheric altitudes, a typical thundercloud produces an insignificant electrostatic field whereas a giant thundercloud can drive the horizontal electrostatic field with a magnitude of ~270 μV/m for nighttime conditions.
Vitaly P. Kim,Valery V. Hegai 한국우주과학회 2015 Journal of Astronomy and Space Sciences Vol.32 No.2
In this paper we study the transmission of the electrostatic field due to coulomb charges of an individual thundercloud into the midlatitude ionosphere, taking into account the total geomagnetic field integrated Pedersen conductivity of the ionosphere. It is shown that at ionospheric altitudes, a typical thundercloud produces an insignificant electrostatic field whereas a giant thundercloud can drive the horizontal electrostatic field with a magnitude of ~270 μV/m for nighttime conditions.
Low Latitude Plasma Blobs: A Review
Vitaly P. Kim,Valery V. Hegai 한국우주과학회 2016 Journal of Astronomy and Space Sciences Vol.33 No.1
In recent years, there has been renewed activity in the study of local plasma density enhancements in the low latitude F region ionosphere (low latitude plasma blobs). Satellite, all-sky airglow imager, and radar measurements have identified the characteristics of these blobs, and their coupling to Equatorial Plasma Bubbles (EPBs). New information related to blobs has also been obtained from the Communication/Navigation Outage Forecasting System (C/NOFS) satellite. In this paper, we briefly review experimental, theoretical and modeling studies related to low latitude plasma blobs.
On the Variability of the Ionospheric F2-Layer During the Quietest Days in December 2009
Vitaly P. Kim,Valery V. Hegai 한국우주과학회 2016 Journal of Astronomy and Space Sciences Vol.33 No.4
December 2009 was one of the quietest (monthly Ap=2) months over the last eight decades. It provided an excellent opportunity to study the day-to-day variability of the F2 layer with the smallest contribution due to geomagnetic activity. With this aim, we analyze hourly values of the F2-layer critical frequency (foF2) recorded at 18 ionosonde stations during the magnetically quietest (Ap=0) days of the month. The foF2 variability is quantified as the relative standard deviation of foF2 about the mean of all the “zero-Ap” days of December 2009. This case study may contribute to a more clear vision of the F2-layer variability caused by sources not linked to geomagnetic activity. In accord with previous studies, we find that there is considerable “zero-Ap” variability of foF2 all over the world. At most locations, foF2 variability is presumably affected by the passage of the solar terminator. The patterns of foF2 variability are different at different stations. Possible causes of the observed diurnal foF2 variability may be related to “meteorological” disturbances transmitted from the lower atmosphere or/and effects of the intrinsic turbulence of the ionosphere-atmosphere system.
Vitaly P. Kim,Valery V. Hegai,Jann Yenq Liu,류광선,정종균 한국우주과학회 2017 Journal of Astronomy and Space Sciences Vol.34 No.4
The electric coupling between the lithosphere and the ionosphere is examined. The electric field is considered as a timevarying irregular vertical Coulomb field presumably produced on the Earth’s surface before an earthquake within its epicentral zone by some micro-processes in the lithosphere. It is shown that the Fourier component of this electric field with a frequency of 500 Hz and a horizontal scale-size of 100 km produces in the nighttime ionosphere of high and middle latitudes a transverse electric field with a magnitude of ~20 mV/m if the peak value of the amplitude of this Fourier component is just 30 V/m. The time-varying vertical Coulomb field with a frequency of 500 Hz penetrates from the ground into the ionosphere by a factor of ~7×105 more efficient than a time independent vertical electrostatic field of the same scale size. The transverse electric field with amplitude of 20 mV/m will cause perturbations in the nighttime F region electron density through heating the F region plasma resulting in a reduction of the downward plasma flux from the protonosphere and an excitation of acoustic gravity waves.
Kim, Vitaly P.,Hegai, Valery V. The Korean Space Science Society 2015 Journal of Astronomy and Space Sciences Vol.32 No.2
In this paper we study the transmission of the electrostatic field due to coulomb charges of an individual thundercloud into the midlatitude ionosphere, taking into account the total geomagnetic field integrated Pedersen conductivity of the ionosphere. It is shown that at ionospheric altitudes, a typical thundercloud produces an insignificant electrostatic field whereas a giant thundercloud can drive the horizontal electrostatic field with a magnitude of ${\sim}270{\mu}V/m$ for nighttime conditions.
Vitaly P. Kim,Valery V. Hegai 한국우주과학회 2015 Journal of Astronomy and Space Sciences Vol.32 No.4
In this study, we documented the midlatitude F2-layer response to five strong geomagnetic storms with minimum Dst < –150 nT that occurred in solar minimum years using hourly values of the F2-layer critical frequency (foF2) from four ionosondes located in different hemispheres. The results were very limited, but they illustrated some peculiarities in the behavior of the F2-layer storm. During equinox, the characteristic ionospheric disturbance patterns over the Japanese station Wakkanai in the Northern Hemisphere and the Australian station Mundaring in the Southern Hemisphere were consistent with the well-known scenario by Prölss (1993); however, during a December solstice magnetic storm, both stations did not observe any noticeable positive ionospheric disturbances. Over the “near-pole” European ionosonde, clear positive ionospheric storms were not observed during the events, but the “far-from-pole” Southern Hemisphere station Port Stanley showed prominent enhancements in F2-layer peak electron density in all magnetic storms except one. No event produced noticeable nighttime enhancements in foF2 over all four ionosondes.
Valery V. Hegai,Vitaly P. Kim,Anna D. Legen’ka 한국우주과학회 2017 Journal of Astronomy and Space Sciences Vol.34 No.1
The F2-layer critical frequency (foF2) data from several ionosondes are employed to study the long-distance effect of the M8.8 Chile Earthquake of February 27, 2010, on the F2 layer. Significant perturbations of the peak F2-layer electron density have been observed following the earthquake at two South African stations, Hermanus and Madimbo, which are located at great circle distances of ~8,000 and ~10,000 km from the earthquake epicenter, respectively. Simplified estimates demonstrate that the observed ionospheric perturbations can be caused by a long-period acoustic gravity wave produced in the F-region by the earthquake.
Valery V. Hegai,Vitaly P. Kim 한국우주과학회 2016 Journal of Astronomy and Space Sciences Vol.33 No.3
Under the assumption of the presence of a medium-scale E × B drift vortex of plasma in the daytime midlatitude F region, and using a simplified ionospheric model, we demonstrate that the E × B drift produces noticeable perturbations in the horizontal distribution of the plasma density in the upper F region. The pattern of ion density perturbations shows two separate medium scale domains of enhanced and reduced ion density with respect to the background. The E × B drift does not produce multiple small-scale ion density irregularities through plasma mixing because of the suppression effect of the field-aligned ambipolar plasma diffusion.
로켓엔진의 극저온 연료 공급관내에서 기체상 응축에 관한 연구
비탈리 A. 베르샤드시키(Vitaly A. Bershadskiy),김철웅(Cheul Woong Kim),발레리 P. 피르소프(Valery P. Phyrsov),조기주(Kie Joo Cho),오승협(Seung Hyub Oh) 한국항공우주학회 2007 韓國航空宇宙學會誌 Vol.35 No.3
본 연구는 공급계 관에서 극저온 연료의 일부가 기화될 경우에 로켓엔진이 지속적으로 작동될 수 있는지의 여부를 묻는 문제와 관련되어 있다. 유동장 내에 증기가 발생하는 것을 모사하는 실험의 결과분석으로 관내의 압력조건에서 극저온 유체의 온도가 포화온도 보다 낮을 경우 발생된 증기가 완전히 응축될 수 있다는 것을 확인하였다. 극저온 유체의 정상유동에서 비평형 응축영역을 계산하기 위한 경험관계식을 무차원형태로 구하였고, 이 경험관계식이 실제적으로 활용 될 수 있는 분야를 제시하였다. This article is related to the possibility for continuous operation of a liquid rocket engine when a portion of cryogenic propellant in the pipeline is vaporized. As a result of experimental studies imitating the formation of vapors in the flow, we confirmed the possibility of full gas-phase condensation in case temperature of cryogenic liquid is lower than it’s saturation temperature in the pipeline. Empirical equation allowing to calculate a nonequilibrium condensation region in the steady flow of cryogenic liquid was obtained as a non-dimensional form and the fields of practical application were suggested.