Modeling of Propagation of Coronal Mass Ejections Using Interplanetary Scintillation Data

P. Manoharan
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Abstract

This talk reviews the interplanetary scintillation (IPS) technique, which allows for the determination of speed and density turbulence of the solar wind in the three-dimensional (3D) inner heliosphere. When sufficient number of scintillating sources are employed to suitably probe a given part of interplanetary space, IPS observations are powerful to study the ambient solar wind as well as to track coronal mass ejections (CMEs) in the distance range of Sun to Earth's orbit. A number of CMEs have been tracked over the entire Sun-Earth distance, by combining the white-light images from the LASCO/SOHO space mission and IPS measurements obtained from the Ooty Radio Telescope (ORT) and ISEE Multi-antenna system. Since the IPS observations at Ooty are on a grid of large number of radio sources, they provide image of disturbance associated with the CME at different distances from the Sun before its arrival at the near-Earth space. The results on the CME “speeddistance” evolution indicate a two-level deceleration: a low decline in speed at distances within or about 100 solar radii and a rapid decrease at larger distances from the Sun. However, the radial decline rates of speed, respectively within and above 100 solar radii, differ between different CMEs and suggest the involvement of input energy associated with the CME eruption in the propagation as well as the dynamics of the ambient solar wind. The typical linear size evolution of the CME with heliocentric distance suggests a pressure balance maintained between the CME driver gas and the ambient solar wind. Further, IPS estimates of density turbulence and speed have been used as inputs to the University of California, San Diego (UCSD) timedependent tomography to reconstruct the full 3D distributions of both solar wind speed and density throughout the inner heliosphere. The usefulness of IPS measurements is discussed on the possibility of forming a basic model to forecast the arrival of CMEs at 1 AU.
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利用行星际闪烁数据模拟日冕物质抛射的传播
本次演讲回顾了行星际闪烁(IPS)技术,该技术允许在三维(3D)内日球层中确定太阳风的速度和密度。当使用足够数量的闪烁源来适当探测行星际空间的给定部分时,IPS观测对于研究环境太阳风以及跟踪太阳到地球轨道距离范围内的日冕物质抛射(cme)是强有力的。通过结合LASCO/SOHO太空任务的白光图像和oty射电望远镜(ORT)和ISEE多天线系统获得的IPS测量数据,在整个太阳-地球距离上跟踪了许多cme。由于Ooty的IPS观测是在大量射电源的网格上进行的,因此它们提供了CME到达近地空间之前与太阳不同距离的扰动图像。CME“速度-距离”演化的结果表明了两级减速:在距离太阳100倍半径以内的地方速度下降较低,在距离太阳较远的地方速度下降较快。然而,在100太阳半径以内和100太阳半径以上的径向速度下降率在不同的CME之间是不同的,这表明与CME喷发相关的输入能量参与了传播以及周围太阳风的动力学。CME随日心距离的线性演化表明CME驱动气体和周围太阳风之间的压力保持平衡。此外,IPS对密度湍流和速度的估计已被用作加利福尼亚大学圣地亚哥分校(UCSD)的时间相关断层扫描的输入,以重建整个内日球层太阳风速度和密度的完整3D分布。讨论了IPS测量的有用性,讨论了形成一个基本模型来预测cme到达1au的可能性。
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