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Alfven Profile In The Lower Corona: Implications For Shock Formation

机译:下部电晕的Alfven剖面:对冲击形成的影响

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摘要

Observations of type II radio bursts and energetic electron events indicate that shocks can form at 1 -3 solar radii and are responsible for the GeV nucleon~(-1) energies observed in ground level solar energetic particle (SEP) events. Here we provide the first study of the lower corona produced from 10 state-of-the-art models. In particular, we look to the Alfven speed profiles as the criterion for shock formation, independent of exciting agent (e.g., flares and CMEs). Global magnetohydrodynamic models produce Alfven speed profiles that are in conflict with observations: (1) multiple SEP events are observed with a single exciting agent, but most profiles are missing the "hump" required to form multiple shocks; and (2) few slow CMEs cause large SEP events, but most profiles drop very quickly, allowing all slow CMEs to drive strong shocks to form between 1 and 3 R_☉. Simplified Alfven wave-driven wind models have steeper profiles, but are still in disagreement with multiple shock formation. Only studies that include Alfven waves with physically based damping are in agreement with observations. This implies the results of these one-dimensional local studies must be included in global models before we can study shock formation in the lower corona.
机译:对II型无线电脉冲爆发和高能电子事件的观察表明,震动可以在1 -3太阳半径处形成,并与在地面太阳高能粒子(SEP)事件中观察到的GeV核子〜(-1)能量有关。在这里,我们对由10种最新模型产生的下部电晕进行了首次研究。尤其是,我们将Alfven速度曲线作为形成冲击的标准,而与激发剂(例如火炬和CME)无关。全球磁流体动力学模型产生的Alfven速度廓线与观测值相冲突:(1)在单个激发剂的作用下观测到多个SEP事件,但是大多数廓线都缺少形成多次冲击所需的“驼峰”; (2)很少的慢速CME引起大的SEP事件,但是大多数配置文件下降得非常快,从而使所有慢速的CME都可以在1至3R_☉之间形成强烈的冲击。简化的Alfven波浪驱动的风模型具有更陡峭的轮廓,但在多重冲击形成方面仍然存在分歧。只有包含基于物理阻尼的Alfven波的研究才与观测结果一致。这意味着这些一维局部研究的结果必须包含在整体模型中,然后才能研究下部电晕的冲击形成。

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