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首页> 外文期刊>Annales Geophysicae >Radial and latitudinal dependencies of discontinuities in the solar wind between 0.3 and 19 AU and −80° and +10°
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Radial and latitudinal dependencies of discontinuities in the solar wind between 0.3 and 19 AU and −80° and +10°

机译:太阳风在0.3和19 AU之间以及− 80°和+ 10°之间的不连续性的径向和纬度相关性

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摘要

Directional discontinuities (DD) from 5 missions at 7 different locations between 0.3 and 19 AU and −80° and +10° in the 3D heliosphere are investigated during minimum solar activity. The data are surveyed using the identification criteria of Burlaga (1969) (B) and Tsurutani and Smith (1979) (TS). The rate of occurrence depends linearly on the solar wind velocity caused by the geometric effect of investigating a larger plasma volume if the solar wind velocity νsw increases. The radial dependence is proportional to r–0.78 (TS criterion) and r–1.28 (B criterion), respectively. This dependence is not only due to an increasing miss rate with increasing distance. The DDs must be unstable or some other physical effect must exist. After normalization of the daily rates to 400 km/s and 1 AU, no dependence on heliographic latitude or on solar wind structures is observable. This means that the DDs are uniformly distributed on a spherical shell. Normalized 64 DD per day are identified with both criteria. But large variations of the daily rate still occur, indicating that other influences must exist. The ratio of the rates of rotational (RDs) and tangential discontinuities (TDs) depends on the solar wind structures. In high speed streams, relatively more RDs exist than in low speed streams. In the inner heliosphere (r < 10 AU), no radial or latitudinal dependence of the portions of the DD types occur. 55% clear RDs, 10% clear TDs and 33% EDs (either discontinuities) are observed, but the portions differ with regard to the criteria used. In the middle heliosphere (10 AU< r < 40 AU), the DD types are more uniformly distributed. The distribution of the directional change ω over the transition evolves to an increase of smaller ω with increasing distance from the sun. The evolution is yielded by the anisotropic RDs with small ω. The spatial thickness dkm in kilometers increases with distance. The thickness drg normalized to the proton gyro radius decreases by a factor of 50 between 0.3 and 19 AU, from 201.3 rg down to 4.3 rg. In the middle heliosphere, the orientation of the normals relative to the local magnetic field is essentially uniform except for the parallel direction where no DDs occur. This indicates that RDs propagating parallel to B play a special role. In addition, in only a few cases is [υ] parallel to [B / ρ], which is required by the MHD theory for RDs. The DDs have strongly enhanced values of proton gyro radius rg for ω ~ 90°. In contrast, in the inner heliosphere, only a small increase in rg with ω is observed.Key words. Interplanetary physics (discontinuities; interplanetary magnetic fields) – Space plasma physics (discontinuities)
机译:在最小太阳活动期间,研究了3个3D太阳圈中在0.3和19 AU之间以及-80°和+ 10°之间的7个不同位置的5个任务的方向不连续性(DD)。使用Burlaga(1969)(B)和Tsurutani and Smith(1979)(TS)的识别标准对数据进行调查。如果太阳风速ν sw 增加,则发生率线性依赖于研究更大等离子体体积的几何效应引起的太阳风速。径向相关性与 r –0.78 (TS准则)和 r –1.28 (B准则)成正比,分别。这种依赖性不仅是由于错过距离随着距离的增加而增加。 DD必须不稳定或必须存在其他物理影响。将日速率归一化至400 km / s和1 AU后,就看不到对仰角纬度或太阳风结构的依赖。这意味着DD均匀分布在球形外壳上。使用这两个标准可以确定每天标准化的64 DD。但是,日费率仍会发生很大变化,这表明还必须存在其他影响。旋转速率(RDs)和切向不连续速率(TDs)的比率取决于太阳风的结构。在高速流中,与低速流中相比,存在相对更多的RD。在内部日球层( r <10 AU)中,没有发生DD类型部分的径向或纬度依赖性。观察到55%的透明RD,10%的透明TD和33%的ED(均不连续),但是这些部分在所使用的标准方面有所不同。在中日球(10 AU r <40 AU)中,DD类型分布更均匀。方向变化ω在过渡过程中的分布随着距太阳的距离增加而逐渐变小。演化是由ω小的各向异性RD产生的。以千米为单位的空间厚度 d km 随着距离的增加而增大。归一化为质子陀螺半径的厚度 d rg 从201.3 r g 减小了0.3到19 AU之间的50倍。 降至4.3 r g 。在中日球层中,法线相对于局部磁场的方向基本一致,除了没有DD出现的平行方向外。这表明平行于 B 传播的RD发挥了特殊作用。另外,在少数情况下,[υ]与[ B / ρ]平行,即MHD理论对RD的要求。在ω〜90°时,DDs的质子陀螺半径 r g 值大大增强。相反,在内部日球层中,仅观察到 r g 随着ω的微小增加。 关键字行星际物理学(间断性;行星际磁场)–空间等离子体物理学(间断性)

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