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首页> 外文期刊>The Astrophysical journal >TWO-DIMENSIONAL STRUCTURE OF A POLAR CORONAL HOLE AT SOLAR MINIMUM: NEW SEMIEMPIRICAL METHODOLOGY FOR DERIVING PLASMA PARAMETERS
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TWO-DIMENSIONAL STRUCTURE OF A POLAR CORONAL HOLE AT SOLAR MINIMUM: NEW SEMIEMPIRICAL METHODOLOGY FOR DERIVING PLASMA PARAMETERS

机译:极小值的冠冕孔的二维结构:推导等离子体参数的新半对称方法

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We develop a new technique to determine the plasma parameters in a polar coronal hole. This method makes use of the line intensities of the H Ⅰ Lyα λ1215.6 line and of the O Ⅵ λλ1031.9, 1037.6 doublet, measured with the Ultraviolet Coronagraph Spectrometer (UVCS) on board the ESA-NASA solar spacecraft Solar and Heliospheric Observatory (SOHO) during 1996 August. The observed intensities are self-consistently reproduced with a two-dimensional semiempirical coronal hole model, for heliocentric distances between 1.4 and 2.6 solar radius and latitudes between 90° (north pole) and 40° Electron densities are derived by separating the O Ⅵ doublet collisional components from those due to resonant scattering. The calculated electron density radial profiles are consistent with typical polar coronal hole data and show only a moderate increase with latitude decreasing, in regions close to the equatorial streamer. The outflow speeds of protons and O Ⅵ ions are determined by means of the Doppler dimming technique. In the Doppler dimming analysis we use kinetic temperatures T_k derived from UVCS observations of the line profiles, whenever available, or we keep T_k as a free parameter if not provided by data. Mass flux conservation along the magnetic field lines is studied adopting a simple analytical model for the geometry of the magnetic flux tubes. Our model shows that protons and O Ⅵ ions accelerate outward, but their outflow speed turns out to decrease slowly as latitude decreases. The O Ⅵ speed, initially comparable to the speed of protons, exceeds the proton speed beyond ~ 1.7 solar radius. Anisotropic O Ⅵ kinetic temperatures, T_‖ and T_⊥, turn out to be necessary to ensure the consistency of the model parameters with mass flux conservation, while the H kinetic temperature distribution is kept isotropic. Results from our model are compared with those from other two-dimensional models recently developed.
机译:我们开发了一种新技术来确定极地冠状孔中的等离子体参数。该方法利用了ESA-NASA太阳航天器太阳和日球天文台上的紫外线电晕光谱仪(UVCS)测量的HⅠLyαλ1215.6线和OⅥλλ1031.9、1037.6 doublet的线强度。 (SOHO)在1996年8月。观测到的强度是通过二维半经验日冕孔模型自洽地再现的,其中日心距为1.4至2.6太阳半径,纬度为90°(北极)与40°之间。电子密度是通过分离OⅥ双峰碰撞得到的那些来自共振散射的成分。计算得出的电子密度径向剖面与典型的极地冠冕孔数据一致,并且在赤道拖缆附近区域随纬度的减小仅显示出适度的增加。质子和OⅥ离子的流出速度通过多普勒调光技术确定。在多普勒调光分析中,我们会使用从线轮廓的UVCS观测值得出的动力学温度T_k(如果有),或者将T_k保留为自由参数(如果数据未提供)。通过对磁通管的几何形状采用简单分析模型,研究了沿磁力线的质量通量守恒。我们的模型表明,质子和OⅥ离子向外加速,但它们的流出速度却随着纬度的减小而缓慢减小。 OⅥ速度最初可与质子速度相媲美,超过质子速度超过〜1.7太阳半径。为了确保模型参数与质量通量守恒相一致,必须保证各向异性的OⅥ动力学温度T_‖和T_⊥,同时保持H动力学温度分布各向同性。我们的模型结果与最近开发的其他二维模型的结果进行了比较。

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