论文标题
增强的质子平行温度在内部层中折返的斑块内部
Enhanced proton parallel temperature inside patches of switchbacks in the inner heliosphere
论文作者
论文摘要
折返是在整个地球层中观察到的太阳风磁场中的离散角偏转。帕克太阳能探测器(PSP)的最新观察结果表明,在小时到几天的规模上存在斑块,并以“安静”的径向场隔开。我们旨在使用质子温度各向异性的测量结果进一步诊断这些斑块的起源,该质子温度各向异性可以照亮与太阳能电晕中的形成过程的可能链接。我们将3D Bi-Maxwellian功能拟合到由Span-Ai仪器在板上PSP上测量的质子速度分布的核心,以获得质子平行的$ T_ {P,\ |} $和垂直,$ t_ {p,p,\ perp} $,温度。我们表明,斑块的存在是由流动和磁场中远离径向方向的横向偏转突出的。这些偏转与$ t_ {p,\ |} $中的增强功能相关,而$ t_ {p,\ perp} $保持相对恒定。斑块有时会显示出小质子和电子密度增强。我们解释说,补丁不仅仅是一组折返,而是将折返嵌入了由增强的$ t_ {p,\ |} $确定的较大规模结构中,与周围的太阳风不同。我们建议这些观察结果与Corona中与重新连接相关的机制形成一致。
Switchbacks are discrete angular deflections in the solar wind magnetic field that have been observed throughout the heliosphere. Recent observations by Parker Solar Probe (PSP) have revealed the presence of patches of switchbacks on the scale of hours to days, separated by 'quieter' radial fields. We aim to further diagnose the origin of these patches using measurements of proton temperature anisotropy that can illuminate possible links to formation processes in the solar corona. We fitted 3D bi-Maxwellian functions to the core of proton velocity distributions measured by the SPAN-Ai instrument onboard PSP to obtain the proton parallel, $T_{p,\|}$, and perpendicular, $T_{p,\perp}$, temperature. We show that the presence of patches is highlighted by a transverse deflection in the flow and magnetic field away from the radial direction. These deflections are correlated with enhancements in $T_{p,\|}$, while $T_{p,\perp}$ remains relatively constant. Patches sometimes exhibit small proton and electron density enhancements. We interpret that patches are not simply a group of switchbacks, but rather switchbacks are embedded within a larger-scale structure identified by enhanced $T_{p,\|}$ that is distinct from the surrounding solar wind. We suggest that these observations are consistent with formation by reconnection-associated mechanisms in the corona.