• 한국우주과학회:학술대회논문집(한국우주과학회보)
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• 한국우주과학회 1993년도 한국우주과학회보 제2권2호
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• pp.8-8
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• 1993

Field-aligned(Birkeland) currents of the High-latitude polar region are to the linkage between the solar wind-magnetosphere system and the ionosphere. The characteristics of field-aligned currents at an attitude of 1300 km have been investigated from the KiSat-A satellite magnetometer data recorded at SatRec form March to May 1993. It is found that the po1arity of both east-west and south-north magnetic components becomes reversed and distorted across the poleward edge. We suggest that these changes May occur rule to the Region 1 and Region 2 currents. It is also suggested that the current time resolution which is about 30 seconds, should be improved to prove gradual polarity changes in the polar region. In addition, it is shown how the observational results depend on the longitude in the high-latitude region.

• Journal of Astronomy and Space Sciences
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• 제39권3호
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• pp.79-86
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• 2022

Thermospheric wind observations from high to mid latitudes are compared with the newly developed Multiscale Atmosphere Geospace Environment (MAGE) model for the Nov 3-4 geomagnetic storm. The observation and simulation comparison shows a very good agreement and is better at high latitudes in general. We were able to identify a thermospheric poleward wind reduction possibly linked to a northward turning of the Interplanetary Magnetic Field (IMF) at ~22 UT on Nov 3 and an enhancement of the poleward wind to a southward turning near 10 UT on Nov 4 at high latitudes. An IMF southward turning may have led to an enhancement of equatorward winds at Boulder, Colorado near midnight. Simultaneous occurrence of aurora may be associated with an IMF By turning negative. The MAGE model wind simulations are consistent with observations in these cases. The results show the model can be a very useful tool to further study the magnetosphere and ionosphere coupling on short time scales.

• 천문학회보
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• 제46권1호
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• pp.58.4-59
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• 2021

This presentation introduces Korea's SNIPE (Small scale magNespheric and Ionospheric Plasma Experiment) mission, formation flying CubeSat constellation. Observing particles and waves on a single satellite suffers from inherent space-time ambiguity. To observe spatial and temporal variations of the micro-scale plasma structures on the topside ionosphere, four 6U CubeSats (~ 10 kg) will be launched into a polar orbit of the altitude of ~500 km in 2021. The distances of each satellite will be controlled from 10 km to more than 100 km by formation flying algorithm. The SNIPE mission is equipped with identical scientific instruments, solid-state telescope, magnetometer, and Langmuir probe. All the payloads have a high temporal resolution (sampling rates of about 10 Hz). Iridium modules provide an opportunity to upload changes in operational modes when geomagnetic storms occur. SNIPE's observations of the dimensions, occurrence rates, amplitudes, and spatiotemporal evolution of polar cap patches, field-aligned currents (FAC), radiation belt microbursts, and equatorial and mid-latitude plasma blobs and bubbles will determine their significance to the solar wind-magnetosphere-ionosphere interaction and quantify their impact on space weather.

• 천문학회보
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• 제46권2호
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• pp.35.1-35.1
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• 2021

Variability in young stellar objects (YSOs) can be caused by various time-dependent phenomena associated with star formation, including accretion rates, geometric changes in the circumstellar disks, stochastic hydromagnetic interactions between stellar surfaces and inner disk edges, reconnections within the stellar magnetosphere, and hot/cold spots on stellar surfaces. Among these YSO variability phenomena, bursts of accretion, which are the most remarkable variability, usually occur sporadically, making it challenging to catch the bursting moments observationally. However, the burst accretion process significantly affects the chemical conditions of the disk and envelope of a YSO, which can be used as a prominent tracer of episodic accretion. I will introduce our ensemble studies of YSO variability at mid-IR and submillimeter and also cover the ALMA observations of several YSOs in the burst accretion phase, especially in the view of chemistry.

• 천문학회지
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• 제56권1호
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• pp.41-57
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• 2023

We measured temporal and emission properties of quiescent magnetars using archival Chandra and XMM-Newton data, produced a list of the properties for 17 magnetars, and revisited previously suggested correlations between the properties. Our studies carried out with a larger sample, better spectral characterizations, and more thorough analyses not only confirmed previously-suggested correlations but also found new ones. The observed correlations differ from those seen in other neutron-star populations but generally accord with magnetar models. Specifically, the trends of the intriguing correlations of blackbody luminosity (L_BB) with the spin-inferred dipole magnetic field strength (B_S) and characteristic age (τ_c) were measured to be L_BB ∝ B^1.5_S and L_BB ∝ τ^-0.6_c, supporting the twisted magnetosphere and magnetothermal evolution models for magnetars. We report the analysis results and discuss our findings in the context of magnetar models.

• Journal of Astronomy and Space Sciences
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• 제28권1호
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• pp.17-26
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• 2011

Bow shock, formed by the interaction between the solar wind and a planet, is generated in different patterns depending on the conditions of the planet. In the case of the earth, its own strong magnetic field plays a critical role in determining the position of the bow shock. However, in the case of Mars of which has very a small intrinsic magnetic field, the bow shock is formed by the direct interaction between the solar wind and the Martian ionosphere. It is known that the position of the Martian bow shock is affected by the mass loading-effect by which the supersonic solar wind velocity becomes subsonic as the heavy ions originating from the planet are loaded on the solar wind. We simulated the Martian magnetosphere depending on the changes of the density and velocity of the solar wind by using the three-dimensional magnetohydrodynamic model built by modifying the comet code that includes the mass loading effect. The Martian exosphere model of was employed as the Martian atmosphere model, and only the photoionization by the solar radiation was considered in the ionization process of the neutral atmosphere. In the simulation result under the normal solar wind conditions, the Martian bow shock position in the subsolar point direction was consistent with the result of the previous studies. The three-dimensional simulation results produced by varying the solar wind density and velocity were all included in the range of the Martian bow shock position observed by Mariner 4, Mars 2, 3, 5, and Phobos 2. Additionally, the simulation result also showed that the change of the solar wind density had a greater effect on the Martian bow shock position than the change of the solar wind velocity. Our result may be useful in analyzing the future observation data by Martian probes.

• Journal of Astronomy and Space Sciences
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• 제14권2호
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• pp.275-285
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• 1997

1989년 2월에 일본의 우주과학연구소(ISAS: Institute of Space and Astronautical Science)에서 발사한 과학위성 EXOS-D의 전기장 측정기와 지자기 자오선 동경 190/210 선상에 위치하고 있는 17개의 지상자력계들로부터 1994년 11월 09일 18시 50분부터 약 20분에 걸쳐 Pi 2 파동이 검출되었다. 우리가 이용한 지상자력계는 지자기 경도는 동경 185.02에서 동경 269.36사이, 지자기 위도는 -37.09에서 65.67사이에, L값은 1.00에서 5.89사이에 위치하고 있다. 또한 같은 시각에 또 다른 위성 ETS-VI의 자기장 측정기의 자료와 지상의 Kakioka(지자기 동경 208.00, 지자기 위도 26.70), Hermanus(지자기 동경 82.97, 지자기 위도 -33.78) 지상자력계의 자료도 함께 사용하여 비교하여 보았다. Pi 2 파동의 주파수를 알아내기 위하여 FFT를 이용하였으며, L값이 2.35인 EXOS-D 위성과 지상자력계들에서는 주파수가 약 25mHz에서 최대 값을 보였으나, L값이 6.60인 ETS-VI위성에서는 같은 주파수가 검출되지 않았다. 또한 지상자력계 중에서 MUT 지상자력계의 자료를 기준으로 하여 위성들과 나머지 지상자력계들간의 상관관계, 위상 차를 조사하여, 발견된 Pi 2 파 동 현상이 플라즈마구 내에서 형성된 공동(cavity) mode에 의한 현상임을 알 수 있었다.

• 우주기술과 응용
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• 제2권2호
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• pp.104-120
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• 2022

도요샛(Small Scale magNetospheric and Ionospheric Plasma Experiment, SNIPE)의 과학임무는 전리권 상층부 소규모 플라즈마 구조의 공간적 시간적 변화를 관찰하는 것이다. 이를 위해 4개의 6U 큐브위성(10 kg)이 고도 약 500 km 극궤도로 발사될 예정이며, 상호 위성 간 거리는 편대 비행 알고리즘에 의해 수 10 km에서 수 1,000 km 이상으로 제어된다. 운영 초기에는 4기의 위성이 같은 궤도 평면에 위치하는 종대비행을 하다가 경도상에서 나란히 배치되는 횡대비행으로 전환하여 4기의 서로 다른 지점에서 공간적인 변화를 관측하게 된다. 도요샛에는 입자 검출기, 랑뮈어 탐침, 자력계로 구성된 우주날씨 관측 장비가 각 위성에 탑재된다. 모든 관측기는 10 Hz 이상의 높은 시간 분해능을 가지며 큐브위성에 최적화 설계되었다. 이 외에도 이리디듐 통신 모듈은 지자기 폭풍이 발생할 때 작동 모드를 변경하기 위한 명령을 업로드할 수 있는 기회를 제공한다. 도요샛은 극 지역 플라즈마 밀도 급상승, 필드 정렬 전류, 고에너지 전자의 국소 영역 침투, 적도 및 중위도 플라즈마 거품의 발생 및 시공간적 진화에 대한 관찰을 수행할 예정이며, 이를 통해 태양풍이 우주날씨에 어떠한 영향을 미치는지 탐구하게 된다. 도요샛은 2023년 상반기 러시아 소유즈-2에 의해 카자흐스탄 바이코누르에서 발사될 예정이다.

• Journal of Astronomy and Space Sciences
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• 제37권2호
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• pp.85-94
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• 2020

Equatorial noise, also known magnetosonic waves (MSWs), are one of the frequently observed plasma waves in Earth's inner magnetosphere. Observations have shown that wave amplitudes maximize at the magnetic equator with a narrow extent in their latitudinal distribution. It has been understood that waves are generated from an equatorial source region and confined within a few degrees magnetic latitude. The present study investigates whether the MSW instability and saturation amplitudes maximize at the equator, given an energetic proton ring-like distribution derived from an observed wave event, and using linear instability analysis and particle-in-cell simulations with the plasma conditions at different latitudes along the dipole magnetic field line. The results show that waves initially grow fastest (i.e., with the largest growth rate) at high latitude (20°-25°), but consistent with observations, their saturation amplitudes maximize within ±10° latitude. On the other hand, the slope of the saturation amplitudes versus latitude revealed in the present study is not as steep as what the previous statistical observation results suggest. This may be indicative of some other factors not considered in the present analyses at play, such as background magnetic field and plasma inhomogeneities and the propagation effect.

• Journal of Astronomy and Space Sciences
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• 제37권2호
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• pp.77-84
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• 2020

We performed high-resolution three-dimensional global magnetohydrodynamic (MHD) simulations to study the interaction between the Earth's magnetosphere and a prolonged steady southward interplanetary magnetic field (IMF) (Bz = -2nT) and slow solar wind. The simulation results show that dayside magnetic reconnection continuously occurs at the subsolar region where the magnetosheath magnetic field is antiparallel to the geomagnetic field. The plasmoid developed on closed plasma sheet field lines. We found that the vortex was generated at the magnetic equator such as (X, Y) = (7.6, 8.9) R_E due to the viscous-like interaction, which was strengthened by dayside reconnection. The magnetic field and plasma properties clearly showed quasiperiodic variations with a period of 8-10 min across the vortex. Additionally, double twin parallel vorticity in the polar region was clearly seen. The peak value of the cross-polar cap potential fluctuated between 17 and 20 kV during the tail reconnection.