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Physical Conditions in the Chromosphere of a Two-Strand Solar Flare with Ejection

机译:带有喷射的两股太阳耀斑在色球中的物理条件

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Chromosphere layers of solar flares were investigated according to the observed profiles of the H_α line. A two-strand flare was observed on September 4, 1990. Spectra were obtained with the ATsU-26 solar horizontal telescope at Terskol Peak Observatory (3100 m). Spectra photometry is performed for two bright nodes of one strand of the flare. Some profiles are superposed to the ejection. The observed profiles are characterized by high emissions in the wings of the H_α line (up to 10-12 ?) under relatively low intensity in the center of H_α (r = 0.35-0.6). To explain such profile behavior we calculated flare models with two or three components. Separate components of the model correspond to unresolved details in the flare area and therefore the averaged profile is calculated. Emission in the far wings is explained by model components with deep heating of chromosphere layers. These occupy 5-12% of the total area. Noticeable emission asymmetry is explained by ray velocities of up to 70 km/s and more. The models are determined by agreement of the observed and calculated profiles. We processed several photometric profiles for seven observations. The temperature in the models with deep heating in the lower cromosphere is increased by 1000-2500 K with respect to the model with an undisturbed chromosphere VAL-C. The second feature of the observed profiles is their high asymmetry and shift with respect to the undisturbed profiles. This can be explained by the opposite motion of the material. We revealed that for the most of the profiles the line-of-sight velocities were directed to the observer in the upper chromosphere (10-100 km/s) and from the observer in the lower chromosphere (5-20 km/s).
机译:根据观察到的H_α线剖面研究了耀斑的大气层。 1990年9月4日观察到两束耀斑。光谱是在Terskol Peak天文台(3100 m)用ATsU-26太阳水平望远镜获得的。对一束火炬的两个亮节点执行分光光度法。一些轮廓叠加到弹出上。观测到的剖面特征是在H_α中心的强度相对较低(r = 0.35-0.6)的情况下,H_α线的机翼(高达10-12?)中的高发射。为了解释这种轮廓行为,我们计算了具有两个或三个分量的耀斑模型。模型的单独组成部分对应于耀斑区域中尚未解决的细节,因此将计算出平均轮廓。通过深层色球层加热的模型分量解释了远翼的辐射。这些占总面积的5-12%。高达70 km / s或更高的射线速度解释了明显的发射不对称性。通过观察和计算的轮廓的一致来确定模型。我们为七个观测值处理了几个光度剖面。与色球层VAL-C不受干扰的模型相比,较低层大气深层加热的模型的温度升高了1000-2500K。观察到的轮廓的第二个特征是它们的高度不对称性和相对于未受干扰的轮廓的偏移。这可以通过材料的相反运动来解释。我们发现,对于大多数剖面,视线速度是指向较高色度层(10-100 km / s)的观察者和较低色度层(5-20​​ km / s)的观察者。

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