TRIO (Triplet Ionospheric Observatory) CINEMA

  • Lee, Dong-Hun (School of Space Research, Kyung Hee University) ;
  • Seon, Jong-Ho (School of Space Research, Kyung Hee University) ;
  • Jin, Ho (School of Space Research, Kyung Hee University) ;
  • Kim, Khan-Hyuk (School of Space Research, Kyung Hee University) ;
  • Lee, Jae-Jin (Korea Astronomy and Space Science Institute) ;
  • Jeon, Sang-Min (School of Space Research, Kyung Hee University) ;
  • Pak, Soo-Jong (School of Space Research, Kyung Hee University) ;
  • Jang, Min-Hwan (School of Space Research, Kyung Hee University) ;
  • Kim, Kap-Sung (School of Space Research, Kyung Hee University) ;
  • Lin, R.P. (School of Space Research, Kyung Hee University) ;
  • Parks, G.K. (Space Science Lab, UC Berkeley) ;
  • Halekas, J.S. (Space Science Lab, UC Berkeley) ;
  • Larson, D.E. (Space Science Lab, UC Berkeley) ;
  • Eastwood, J.P. (Space Science Lab, UC Berkeley) ;
  • Roelof, E.C. (Applied Physics Lab, Johns Hopkins University) ;
  • Horbury, T.S. (Blackett Lab, Imperial College)
  • 발행 : 2009.10.15

초록

Triplets of identical cubesats will be built to carry out the following scientific objectives: i) multi-observations of ionospheric ENA (Energetic Neutral Atom) imaging, ii) ionospheric signature of suprathermal electrons and ions associated with auroral acceleration as well as electron microbursts, and iii) complementary measurements of magnetic fields for particle data. Each satellite, a cubesat for ion, neutral, electron, and magnetic fields (CINEMA), is equipped with a suprathermal electron, ion, neutral (STEIN) instrument and a 3-axis magnetometer of magnetoresistive sensors. TRIO is developed by three institutes: i) two CINEMA by Kyung Hee University (KHU) under the WCU program, ii) one CINEMA by UC Berkeley under the NSF support, and iii) three magnetometers by Imperial College, respectively. Multi-spacecraft observations in the STEIN instruments will provide i) stereo ENA imaging with a wide angle in local times, which are sensitive to the evolution of ring current phase space distributions, ii) suprathermal electron measurements with narrow spacings, which reveal the differential signature of accelerated electrons driven by Alfven waves and/or double layer formation in the ionosphere between the acceleration region and the aurora, and iii) suprathermal ion precipitation when the storm-time ring current appears. In addition, multi-spacecraft magnetic field measurements in low earth orbits will allow the tracking of the phase fronts of ULF waves, FTEs, and quasi-periodic reconnection events between ground-based magnetometer data and upstream satellite data.

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