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Proton cyclotron waves upstream from Mars: Observations from Mars Global Surveyor

机译:火星上游的质子回旋波:火星全球测量师的观测

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We present a study on the properties of electromagnetic plasma waves in the region upstream of the Martian bow shock, detected by the magnetometer and electron reflectometer (MAG / ER) onboard the Mars Global Surveyor (MGS) spacecraft during the period known as Science Phasing Orbits (SPO). The frequency of these waves, measured in the MGS reference frame (SC), is close to the local proton cyclotron frequency. Minimum variance analysis (MVA) shows that these 'proton cyclotron frequency' waves (PCWs) are characterized - in the SC frame - by a left-hand, elliptical polarization and propagate almost parallel to the background magnetic field. They also have a small degree of compressibility and an amplitude that decreases with the increase of the interplanetary magnetic field (IMF) cone angle and radial distance from the planet. The latter result supports the idea that the source of these waves is Mars. In addition, we find that these waves are not associated with the foreshock and their properties (ellipticity, degree of polarization, direction of propagation) do not depend on the IMF cone angle. Empirical evidence and theoretical approaches suggest that most of these observations correspond to the ion-ion right hand (RH) mode originating from the pick-up of ionized exospheric hydrogen. The left-hand (LH) mode might be present in cases where the IMF is almost perpendicular to the Solar Wind direction. PCWs occur in 62% of the time during SPO1 subphase, whereas occurrence drops to 8% during SPO2. Also, SPO1 PCWs preserve their characteristics for longer time periods and have greater degree of polarization and coherence than those in SPO2. We discuss these results in the context of possible changes in the pick-up conditions from SPO1 to SPO2, or steady, spatial inhomogeneities in the wave distribution. The lack of influence from the Solar Wind's convective electric field upon the location of PCWs indicates that, as suggested by recent theoretical results, there is no clear relation between the spatial distribution of PCWs and that of pick-up ions.
机译:我们目前对火星全球弓箭仪(MGS)航天器上的磁力计和电子反射计(MAG / ER)探测到的火星弓激波上游区域中的电磁等离子体波的特性进行了研究,该阶段被称为“科学相位轨道” (SPO)。在MGS参考系(SC)中测量的这些波的频率接近于本地质子回旋加速器频率。最小方差分析(MVA)表明,这些“质子回旋频率”波(PCW)在SC帧中的特征是左旋椭圆极化,并且几乎平行于背景磁场传播。它们还具有较小程度的可压缩性,并且振幅随着行星际磁场(IMF)锥角和距行星的径向距离的增加而减小。后者的结果支持了这些波的来源是火星的想法。另外,我们发现这些波与前震无关,并且它们的性质(椭圆度,极化度,传播方向)不依赖于IMF锥角。经验证据和理论方法表明,这些观察结果大多数对应于离子电离层外氢的吸收而产生的离子右手(RH)模式。在IMF几乎垂直于太阳风向的情况下,可能会出现左手(LH)模式。在SPO1子阶段,PCW发生的时间为62%,而在SPO2期间,发生率下降为8%。此外,与SPO2中的PCW相比,SPO1 PCW可以保留较长时间的特性,并且具有更高的极化和相干度。我们在从SPO1到SPO2的拾取条件可能变化,或波分布中稳定的空间不均匀性的背景下讨论这些结果。太阳风的对流电场对PCW的位置没有影响,这表明,正如最近的理论结果所表明的那样,PCW的空间分布与吸收离子的空间分布之间没有明确的关系。

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