Buoyancy Modes in a Low Entropy Bubble

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-11-08 DOI:10.1029/2024JA032714
F. R. Toffoletto, R. A. Wolf, J. Derr
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Abstract

In the nightside region of Earth's magnetosphere, braking oscillations or buoyancy modes have been associated with the occurrence of low entropy bubbles. These bubbles form in the plasma sheet, particularly during geomagnetically disturbed times, and because of interchange, move rapidly earthward and may eventually come to rest in the inner plasma sheet or inner magnetosphere. Upon arrival, they often exhibit damped oscillations with periods of a few minutes and are associated with Pi2 pulsations. Previously we used the thin filament approximation to compare the frequencies and modes of buoyancy waves using magnetohydrodynamic (MHD) ballooning and classic interchange theory. Interchange oscillations differ from the more general MHD oscillations by assuming constant pressure along a magnetic field line. It was determined that MHD ballooning and interchange modes are similar for plasma sheet field lines but differ for field lines that map to the inner magnetosphere. This suggested that the classic interchange formulation was only valid in the plasma sheet. This paper tests the hypothesis that the agreement between MHD ballooning and classic interchange could be restored inside a bubble. We create a small region of entropy depletion in the magnetotail and compare the buoyancy mode properties. At some locations inside the bubble, the MHD ballooning buoyancy modes resemble interchange modes but with lower frequencies than those of the unperturbed background. Unstable modes are found on the earthward edge of the bubble, while at the tailward edge, MHD ballooning predicts a slow mode wave solution not seen in the pure interchange solution.

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低熵气泡中的浮力模式
在地球磁层的夜侧区域,制动振荡或浮力模式与低熵气泡的出现有关。这些气泡在等离子体片中形成,特别是在地磁扰动时期,由于相互交换,气泡迅速向地球移动,并可能最终停留在内层等离子体片或内磁层中。到达后,它们通常会表现出周期为几分钟的阻尼振荡,并与 Pi2 脉动有关。在此之前,我们使用细丝近似法,利用磁流体力学(MHD)气球理论和经典的交换理论比较了浮力波的频率和模式。交换振荡与更一般的 MHD 振荡不同,它假定沿磁场线的压力是恒定的。研究发现,等离子体片磁场线的 MHD 气球模式和互换模式相似,但映射到内部磁层的磁场线的 MHD 气球模式和互换模式不同。这表明经典的互换模式只适用于等离子体片。本文检验了一个假设,即在气泡内部可以恢复 MHD 气球和经典互换模式之间的一致性。我们在磁尾创建了一个小的熵耗区域,并比较了浮力模式的特性。在气泡内的某些位置,MHD气球浮力模式类似于交换模式,但频率低于未受扰动的背景模式。在气泡的向地边缘发现了不稳定模式,而在气泡的尾部边缘,MHD气球预言了一种在纯交换解中看不到的慢模式波解。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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