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Towards Construction of a SolarWind 'Reanalysis' Dataset: Application to the First Perihelion Pass of Parker Solar Probe

机译:朝着建造Solarwind“Reanalysis”数据集:应用于Parker Solar探头的第一次截瘫通行证

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Accurate reconstruction of global solar-wind structure is essential for connecting remote and in situ observations of solar plasma, and hence understanding formation and release of solar wind. Information can routinely be obtained from photospheric magnetograms, via coronal and solar-wind modelling, and directly from in situ observations, typically at large heliocentric distances (most commonly near 1 AU).Magnetogram-constrained modelling has the benefit of reconstructing global solar-wind structure, but with relatively large spatial and/or temporal errors. In situ observations, on the other hand, make accurate temporal measurements of solar-wind structure, but are highly localised. We here use a data assimilative (DA) approach to combine these two sources of information as a first step towards producing a solar-wind "reanalysis" dataset that optimally combines model and observation. The physics of solar wind stream interaction is used to extrapolate in heliocentric distance, while the assumption of steady-state solar-wind structure enables extrapolation in longitude. The major challenge is extrapolating in latitude. Using solar-wind speed during the interval of the first perihelion pass of Parker Solar Probe (PSP) in November 2018 as a test bed, we investigate two approaches. The first is to assume the solar wind is two-dimensional and thus has no latitudinal structure within the ±7° bounded by the heliographic equatorial and ecliptic planes. The second assumes in situ solar-wind observations are representative of some (small) latitudinal range. We show how observations of the inner heliosphere, such as will be provided by PSP, can be exploited to constrain the latitudinal representivity of solar-wind observations to improve future solar-wind reconstruction and space-weather forecasting.
机译:全球太阳能结构的准确重建对于连接远程和原位观察的太阳能等离子体,因此是必不可少的,因此了解太阳风的形成和释放。信息可以常规地从光学磁图中获得,通过冠状和​​太阳能建模,并且直接从原位观察,通常在大型的皮层距离(最常见的1 AU)中.Magnetox的受限建模具有重建全球太阳能的益处结构,但具有相对较大的空间和/或时间错误。另一方面,原位观察,对太阳能结构进行准确的时间测量,但是高度本地化。我们在这里使用数据同化(DA)方法将这两个信息来源结合为生产太阳能“重新分析”数据集的第一步,最佳地结合了模型和观察。太阳风流相互作用的物理学用于推断在天管距离中,而稳态太阳能结构的假设能够经度推断。主要挑战是在纬度推断。在2018年11月作为试验台的帕克太阳能探头(PSP)的第一次帕尔太阳能探测(PSP)的间隔期间使用太阳能速度,我们调查了两种方法。首先是假设太阳脉风是二维的,因此在±7°的±7°内没有延伸结构,由直波跳赤赤道和辉丝平面有±7°。第二种假设原位太阳能 - 风观察是一些(小)纬度范围的代表。我们展示了对内部光圈的观察,例如将由PSP提供的,可以利用太阳能观测的纬度代表,以改善未来的太阳能重建和空间天气预报。

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