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首页> 外文期刊>Annales Geophysicae >Open solar flux estimates from near-Earth measurements of the interplanetary magnetic field: comparison of the first two perihelion passes of the Ulysses spacecraft
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Open solar flux estimates from near-Earth measurements of the interplanetary magnetic field: comparison of the first two perihelion passes of the Ulysses spacecraft

机译:来自行星际磁场近地测量的开放太阳通量估计:尤利西斯号航天器的前两次近日点飞行比较

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摘要

Results from all phases of the orbits of the Ulysses spacecraft have shown that the magnitude of the radial component of the heliospheric field is approximately independent of heliographic latitude. This result allows the use of near-Earth observations to compute the total open flux of the Sun. For example, using satellite observations of the interplanetary magnetic field, the average open solar flux was shown to have risen by 29% between 1963 and 1987 and using the aa geomagnetic index it was found to have doubled during the 20th century. It is therefore important to assess fully the accuracy of the result and to check that it applies to all phases of the solar cycle. The first perihelion pass of the Ulysses spacecraft was close to sunspot minimum, and recent data from the second perihelion pass show that the result also holds at solar maximum. The high level of correlation between the open flux derived from the various methods strongly supports the Ulysses discovery that the radial field component is independent of latitude. We show here that the errors introduced into open solar flux estimates by assuming that the heliospheric field's radial component is independent of latitude are similar for the two passes and are of order 25% for daily values, falling to 5% for averaging timescales of 27 days or greater. We compare here the results of four methods for estimating the open solar flux with results from the first and second pere-helion passes by Ulysses. We find that the errors are lowest (1-5% for averages over the entire perehelion passes lasting near 320 days), for near-Earth methods, based on either interplanetary magnetic field observations or the aa geomagnetic activity index. The corresponding errors for the Solanki et al. (2000) model are of the order of 9-15% and for the PFSS method, based on solar magnetograms, are of the order of 13-47%. The model of Solanki et al. is based on the continuity equation of open flux, and uses the sunspot number to quantify the rate of open flux emergence. It predicts that the average open solar flux has been decreasing since 1987, as is observed in the variation of all the estimates of the open flux. This decline combines with the solar cycle variation to produce an open flux during the second (sunspot maximum) perihelion pass of Ulysses which is only slightly larger than that during the first (sunspot minimum) perihelion pass.
机译:尤利西斯(Elysses)航天器轨道各相的结果表明,日球场径向分量的大小大致与纬度无关。该结果允许使用近地观测来计算太阳的总开放通量。例如,利用卫星对行星际磁场的观测,在1963年至1987年之间,平均开放太阳通量显示出增加了29%,而使用aa地磁指数发现,在20世纪,它又翻了一番。因此,重要的是充分评估结果的准确性,并检查其是否适用于太阳周期的所有阶段。尤利西斯(Elysses)飞船的第一次近日近距离通过接近太阳黑子的最小值,而第二次近日近距离通过的最新数据表明,该结果也保持在太阳最大值。从各种方法得出的开放通量之间的高度相关性有力地支持了尤利西斯的发现,即径向场分量与纬度无关。我们在这里表明,假设日球场的径向分量与纬度无关,则引入开放太阳通量估算中的误差在两次通过中相似,日值约为25%,平均27天时标下降至5%或更高。在这里,我们将四种估算开放太阳通量的方法的结果与来自尤利西斯的第一次和第二次日耳轮掠过的结果进行比较。我们发现,基于行星际磁场观测或aa地磁活动指数,对于近地方法,误差最低(对于整个近日线飞行,平均误差为1-5%,持续近320天)。 Solanki等人的相应错误。 (2000年)模型的数量级为9-15%,对于PFSS方法,基于太阳磁图,模型的数量级为13-47%。 Solanki等人的模型。是基于开放通量的连续性方程,并使用黑子数来量化开放通量的出现率。它预测,自1987年以来,平均开放太阳通量一直在下降,正如所有开放通量估计值的变化所观察到的那样。这种下降与太阳周期变化相结合,在尤利西斯的第二次(太阳黑子)近日通过过程中产生一个开放通量,该通量仅略大于第一次(太阳黑子)近日通过过程中的通量。

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