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The solar wind as seen by SOHO/SWAN since 1996: comparison with SOHO/LASCO C2 coronal densities

机译:自1996年以来sOHO / sWaN所见的太阳风:与   sOHO / LasCO C2冠状密度

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摘要

We update the SOHO/SWAN H Lyman-alpha brightness analysis to cover the1996-2008 time interval. A forward model applied to the intensity maps providesthe latitude and time dependence of the interstellar Hydrogen ionisation rateover more than a full solar cycle. The hydrogen ionisation, being almostentirely due to charge-exchange with solar wind ions, reflects closely thesolar wind flux. Our results show that the solar wind latitudinal structureduring the present solar minimum is strikingly different from the previousminimum, with a much wider slow solar wind equatorial belt which persists untilat least the end of 2008. We compute absolute values of the in-ecliptic Hionisation rates using OMNI solar wind data and use them to calibrate ourionisation rates at all heliographic latitudes. We then compare the resultingfluxes with the synoptic LASCO/C2 electron densities at 6 solar radii. The twotime-latitude patterns are strikingly similar over all the cycle. Thiscomparison shows that densities at 6 solar radii can be used to infer the solarwind type close to its source, with high (resp. low) densities tracing the slow(resp. fast) solar wind, simply because the density reflects at which altitudeoccurs the acceleration. The comparison between the two minima suggests thatthe fast polar wind acceleration occurs at larger distance during the currentminimum compared to the previous one. This difference, potentially linked tothe magnetic field decrease or(and) the coronal temperature decrease should bereproduced by solar wind expansion models.
机译:我们更新了SOHO / SWAN H Lyman-alpha亮度分析以涵盖1996-2008年的时间间隔。应用于强度图的正向模型提供的星际氢电离率的纬度和时间依赖性超过整个太阳周期。氢离子化几乎完全归因于与太阳风离子的电荷交换,它紧密地反射了太阳风通量。我们的结果表明,构成当前最低日数的太阳风纬度与先前的最低值有显着差异,慢风赤道带的宽度要宽得多,该赤道带至少持续到2008年底。我们使用OMNI太阳风数据,并用它们来校准所有纬向纬度的去离子率。然后,我们将产生的通量与6个太阳半径处的天气LASCO / C2电子密度进行比较。在整个周期中,两次纬度模式都极为相似。这种比较表明,可以使用6个太阳半径处的密度来推断太阳风的类型接近其源,高(低)密度可以跟踪缓慢(快速)太阳风,这仅仅是因为密度反映了加速度发生在哪个高度。两种极小值之间的比较表明,与上一极小值相比,当前极小值期间的极地风加速快。这种可能与磁场降低或(和)日冕温度降低有关的差异应通过太阳风膨胀模型来再现。

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