日本地球惑星科学連合2014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-EM08_2PM1] Space Weather and Space Climate

2014年5月2日(金) 14:15 〜 16:00 411 (4F)

コンビーナ:*片岡 龍峰(国立極地研究所)、海老原 祐輔(京都大学生存圏研究所)、草野 完也(名古屋大学太陽地球環境研究所)、清水 敏文(宇宙航空研究開発機構宇宙科学研究所)、三好 由純(名古屋大学太陽地球環境研究所)、浅井 歩(京都大学宇宙総合学研究ユニット)、佐藤 達彦(日本原子力研究開発機構)、陣 英克(情報通信研究機構)、伊藤 公紀(横浜国立大学大学院工学研究院)、宮原 ひろ子(武蔵野美術大学造形学部)、座長:海老原 祐輔(京都大学生存圏研究所)、三好 由純(名古屋大学太陽地球環境研究所)

15:45 〜 16:00

[PEM08-27] 南極昭和基地で観測された中間圏・下部熱圏のNOの変動

礒野 靖子1、*水野 亮1長浜 智生1三好 由純1中村 卓司2片岡 龍峰2堤 雅基2江尻 省2藤原 均3前澤 裕之4上村 美久1 (1.名古屋大学 太陽地球環境研究所、2.国立極地研究所、3.成蹊大学、4.大阪府立大学)

キーワード:Nitric oxide, mesosphere and lower thermosphere, energetic particle precipitation, geomagnetic storm, solar proton event, Antarctica

Energetic particle precipitation (EPP) related to solar proton events or geomagnetic storms induce ion-neutral reactions and change abundance of some minor molecules such as NOx and HOx in the mesosphere and lower thermosphere. To investigate the temporal variations of NO by EPP, we installed a millimeter-wave spectroscopic radiometer at Syowa Station (69.00S, 39.85E), and we have carried out ground-based observations of spectral line of nitric oxide (NO) at 250.796 GHz since January 2012.We obtained 197 and 172 daily averaged NO spectra in 2012 and 2013 (until 30 September; DOY 273), respectively. The daily NO spectra are characterized by narrow line width with a Full-Width-at-Half-Maximum (FWHM) of about 0.5 MHz. These NO spectra are well fitted by a single Gauss function or by a single Lorenz function. From the spectral line shape, we conclude that the NO emitting region is between 75 and 100 km.We found two temporal variation patterns of NO column density. One is a seasonal variation with a maximum in the winter and a minimum in the summer. The column density of NO during the winter was about 4 times larger than that during the summer. This seasonal variation is considered to be related to the atmospheric transport and the NO dissociation by solar radiation. The other is the short-term variation in a timeframe of 5-10 days associated with EPP events such as solar proton events and geomagnetic storms. At Syowa Station, short-term variations were caused mainly by the precipitation of electrons rather than that of protons. In the electron precipitation events, the column density of NO gradually increases just after the main phase of the geomagnetic storm and gradually decreases soon after its peak.One of the short-term events related to a large geomagnetic storm in April 2012 was the most prominent single event among those observed at Syowa Station since January 2012. From the high time resolution (∼ 3-hour) data, we revealed a diurnal tendency that NO column density increased about twice at UT 0, which is interpreted to be caused by the dawn-dusk asymmetry of the precipitated electrons with energies 30-300 keV.