日本地球惑星科学連合2016年大会

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セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM07] Dynamics in magnetosphere and ionosphere

2016年5月24日(火) 15:30 〜 17:00 103 (1F)

コンビーナ:*三好 由純(名古屋大学宇宙地球環境研究所)、田中 良昌(国立極地研究所)、中溝 葵(情報通信研究機構 電磁波計測研究所)、尾崎 光紀(金沢大学理工研究域電子情報学系)、中野 慎也(情報・システム研究機構 統計数理研究所)、堀 智昭(名古屋大学宇宙地球環境研究所)、座長:宮下 幸長(名古屋大学宇宙地球環境研究所)

16:45 〜 17:00

[PEM07-12] Preliminary results of auroral tomography analysis of discrete arcs observed on March 14, 2015

*田中 良昌1小川 泰信1門倉 昭1Gustavsson Bjorn2Partamies Noora3Kauristie Kirsti4Whiter Daniel5Enell Carl-fredrik6Braendstroem Urban7Sergienko Tima7Kozlovsky Alexander8宮岡 宏1Kosch Mike9 (1.国立極地研究所、2.UiT The Arctic University of Norway, Norway、3.The University Centre in Svalbard, Norway、4.Finnish Meteorological Institute, Finland、5.University of Southampton, UK、6.EISCAT Scientific Association、7.Swedish Institute of Space Physics, Sweden、8.Sodankyla Geophysical Observatory, Finland、9.South African National Space Agency, South Africa)

キーワード:aurora, tomography analysis, 3D distribution, ionosphere, EISCAT radar

We conducted a campaign of auroral tomography observation using multi-point imager network and the EISCAT UHF radar in Northern Europe in March, 2015. During this campaign, an auroral breakup was observed at 23:15 UT on March 14 by three all-sky EMCCD imagers and three wide-view CCD imagers. Wavy structure of discrete arcs was often observed around the magnetic zenith at Tromso from 22 to 23 UT and pulsating aurora was observed after the breakup. The monochromatic (427.8 nm) images were taken at a sampling interval of 2 seconds by the three EMCCD imagers and at an interval of 10 seconds by all the six imagers. The EISCAT UHF radar at Tromso measured the ionospheric parameters along the field line at the magnetic zenith from 20 to 24 UT.
We apply the auroral tomography method to these data set to reconstruct reliable three-dimensional distribution of the 427.8 nm emission, that will allow us to investigate quantitatively the following subjects; (1) relation between the 427.8 nm emission and electron density enhancement along the field line, (2) spatial distribution of energy of precipitating electrons in the wavy structure, in particular, relation between the energy of precipitating electrons and thickness of discrete arc, (3) relation between motion of the wavy structure and spatial distribution of the ionospheric conductivity, and (4) spatial and temporal variations of energy distribution of precipitating electrons at the auroral breakup. We present preliminary results from the auroral tomography analysis of the discrete arcs.