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Large amplitude undulations of evening site diffuse aurorae. Optical characteristics and conditions of generation

机译:傍晚地点的大幅度起伏弥散极光。光学特性和产生条件

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Optical characteristics of large amplitude undulations (LAU) of diffuse aurorae observed by all-sky cameras at Kola Peninsula on December 28, 2010 were examined. Both interplanetary medium conditions and characteristics of magnetic activity before and during LAU were analyzed. It was shown that the development of undulations could be activated by sharp short-living of similar to 20 minutes solar wind dynamic pressure impulse and existence of the undulations during about two hours was supported by electric field of stationary magnetospheric convection originated from large smoothly changed southward IMF Bz component of about -12nT. The altitude of undulation luminosity determined by triangulation method was 120 +/- 10 km. The undulations amplitude changed from about 100 to 300 km and the average wavelength was similar to 250 km. The undulations were observed moving westward with the average phase velocity of similar to 0.7 km/s. The pass of DMSP F16 spacecraft just along "the tongue" of undulations showed that the wave of luminosity was located in the region of the predominantly ion (proton) precipitation with the average energy of particles of similar to 18 keV. Rayed auroral structures were observed continuously in the region of diffuse aurorae during time interval of LAU existence. These structures were observed moving westward with the velocity of about 2 km/s that corresponds to the northward electric field of similar to 100 mV/m.
机译:研究了2010年12月28日在科拉半岛的全天照相机观测到的弥散极光的大振幅起伏(LAU)的光学特征。分析了LAU之前和期间的行星际介质条件和磁活动特征。结果表明,起伏的发展可以通过短暂的短寿命(类似于20分钟的太阳风动压冲动)来激活,并且起伏的存在在大约两个小时内得到了稳定的磁层对流电场的支持,这是由于向南平稳变化而产生的IMF Bz分量约为-12nT。通过三角测量法确定的起伏发光度的高度为120 +/- 10km。起伏幅度从大约100 km变为300 km,平均波长类似于250 km。观察到起伏向西移动,平均相速度接近0.7 km / s。 DMSP F16航天器正好沿着起伏的“舌头”通过,表明光度波位于主要是离子(质子)沉淀的区域,平均能量类似于18 keV。在LAU存在的时间间隔内,在弥散性极光区域连续观察到射线极光结构。观察到这些结构以约2 km / s的速度向西移动,这相当于向北电场的100 mV / m。

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