• 제목/요약/키워드: the nightside auroral region

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Analysis of Field-Aligned Currents in the High-Altitude Nightside Auroral Region: Cluster Observation

  • Shin, Youra;Lee, Ensang;Lee, Jae-Jin
    • Journal of Astronomy and Space Sciences
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    • 제36권1호
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    • pp.1-9
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    • 2019
  • In this paper we present analysis of current density when the Cluster spacecraft pass the nightside auroral region at about $4-5R_E$ from the center of Earth. The analysis is made when the inter-spacecraft separation is within 200 km, which allows all four spacecraft to be situated inside the same current sheet. On 22 February 2002, two field-aligned current (FAC) events were observed in both the southern and the northern hemispheres. The FACs were calculated with magnetic field data obtained by the four spacecraft using the Curlometer method. The scales of the FACs along the spacecraft trajectory and the magnitudes were hundreds of kilometers and tens of $nA/m^2$, respectively, and both events were mapped to the auroral region in the ionosphere. We also examined reliability of the results with some parameters, and found that our results are adequately comparable with other studies. Nevertheless, some limitations that decrease the accuracy of current estimation exist.

Observations of the Aurora by Visible All-Sky Camera at Jang Bogo Station, Antarctica

  • Jee, Geonhwa;Ham, Young-Bae;Choi, Yoonseung;Kim, Eunsol;Lee, Changsup;Kwon, Hyuckjin;Trondsen, Trond S.;Kim, Ji Eun;Kim, Jeong-Han
    • Journal of Astronomy and Space Sciences
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    • 제38권4호
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    • pp.203-215
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    • 2021
  • The auroral observation has been started at Jang Bogo Station (JBS), Antarctica by using a visible All-sky camera (v-ASC) in 2018 to routinely monitor the aurora in association with the simultaneous observations of the ionosphere, thermosphere and magnetosphere at the station. In this article, the auroral observations are introduced with the analysis procedure to recognize the aurora from the v-ASC image data and to compute the auroral occurrences and the initial results on their spatial and temporal distributions are presented. The auroral occurrences are mostly confined to the northern horizon in the evening sector and extend to the zenith from the northwest to cover almost the entire sky disk over JBS at around 08 MLT (magnetic local time; 03 LT) and then retract to the northeast in the morning sector. At near the magnetic local noon, the occurrences are horizontally distributed in the northern sky disk, which shows the auroral occurrences in the cusp region. The results of the auroral occurrences indicate that JBS is located most of the time in the polar cap near the poleward boundary of the auroral oval in the nightside and approaches closer to the oval in the morning sector. At around 08 MLT (03 LT), JBS is located within the auroral oval and then moves away from it, finally being located in the cusp region at the magnetic local noon, which indicates that the location of JBS turns out to be ideal to investigate the variabilities of the poleward boundary of the auroral oval from long-term observations of the auroral occurrences. The future plan for the ground auroral observations near JBS is presented.

Variation of Floating Potential in the Topside Ionosphere Observed by STSAT-1

  • Lee, Junhyun;Lee, Ensang;Lee, Jaejin;Kim, Khan-Hyuk;Seon, Jongho;Lee, Dong-Hun;Jin, Ho;Kim, Eung-Hyun;Jeon, Hyun-Jin;Lim, Seong-Bin;Kim, Taeyoun;Jang, Jaewoong;Jang, Kyung-Duk;Ryu, Kwangsun
    • Journal of Astronomy and Space Sciences
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    • 제31권4호
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    • pp.311-315
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    • 2014
  • In this study, we investigated the effect of space plasmas on the floating potential variation of a low-altitude, polar-orbiting satellite using the Langmuir Probe (LP) measurement onboard the STSAT-1 spacecraft. We focused on small potential drops, for which the estimation of plasma density and temperature from LP is available. The floating potential varied according to the variations of plasma density and temperature, similar to the previously reported observations. Most of the potential drops occurred around the nightside auroral region. However, unlike the previous studies where large potential drops were observed with the precipitation of auroral electrons, the potential drops occurred before or after the precipitation of auroral electrons. Statistical analysis shows that the potential drops have good correlation with the temperature increase of cold electrons, which suggests the small potential drops be mainly controlled by the cold ionospheric plasmas.