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Physical Properties of a 2003 April Quiescent Streamer

机译:2003年4月静态流光的物理属性

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In 2003 April, the Ultraviolet Coronagraph Spectrometer (UVCS) on board the Solar and Heliospheric Observatory (SOHO) observed a quiescent streamer in an effort to derive the physical plasma parameters across the streamer and as a function of height (from 1.75 to 5.0 R☉). Values for the electron temperature, proton and O5+ kinetic temperatures, elemental abundances, and O5+ outflow velocity were derived. The presence of the first ionization potential (FIP) effect was also explored. These plasma parameters were compared to those derived for other previously reported active region and quiescent streamers. The photospheric normalized absolute elemental abundances for O, Si, S, Ar, and Fe were derived at 1.75 R☉. The remaining parameters were derived at five heights up to 5.0 R☉. To calculate the electron density above 2.2 R☉ the polarized brightness data from another SOHO instrument, the Large Angle Spectroscopic Coronagraph (LASCO) C2 detector, was employed. The streamer was located above a complex filament structure and had a slightly higher electron temperature compared to what is typically found for quiescent streamers. This streamer did exhibit the customary FIP effect, but no abundance-depleted core typically found for such stable quiescent streamers was detected. The perpendicular kinetic temperature for the protons and the O5+ ions did not vary across the streamer. This differs from two other quiescent streamer comparison cases, in which the O5+ kinetic temperature did decrease at the core structure. The O5+ outflow velocities were similar to those observed in an equatorial streamer from solar minimum.
机译:2003年4月,太阳和日球天文台(SOHO)上的紫外线电晕光谱仪(UVCS)观察了一个静止的拖缆,以求得出拖缆上的物理等离子体参数以及高度的函数(从1.75到5.0R☉ )。得出电子温度,质子和O5 +动力学温度,元素丰度和O5 +流出速度的值。还探讨了第一电离势(FIP)效应的存在。将这些血浆参数与其他先前报道的活性区域和静态流光导出的血浆参数进行了比较。 O,Si,S,Ar和Fe的光球归一化绝对元素丰度在1.75R☉下得出。其余参数是在五个最高5.0R☉的高度处得出的。为了计算高于2.2R☉的电子密度,使用了另一台SOHO仪器(大角度光谱电晕仪(LASCO)C2检测器)的极化亮度数据。该拖缆位于复杂的细丝结构上方,并且与静态拖缆通常所发现的相比,电子温度略高。该拖缆确实表现出惯用的FIP效果,但未检测到通常发现的用于此类稳定静态拖缆的丰度耗尽的岩心。质子和O5 +离子的垂直动力学温度在整个拖缆上没有变化。这与其他两个静态拖缆比较例不同,在静态比较例中,O5 +动力学温度确实在核心结构处降低。 O5 +流出速度与从赤道极光观测到的赤道拖缆中观察到的速度相似。

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