4.2 Article

Coupling Between Alfven Wave and Kelvin-Helmholtz Waves in the Low Latitude Boundary Layer

Journal

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fspas.2021.785413

Keywords

Kelvin-Helmholtz instability; Alfven wave; boundary layer; magnetopause; mode conversion; wave coupling

Funding

  1. United States Department of Energy, Office of Science, Office of Fusion Energy Sciences [DE-AC02-09CH11466]
  2. National Science Foundation (NSF) [AGS1602855, AGS1832207]
  3. National Aeronautics and Space Administration (NASA) [80HQTR18T0066, 80HQTR19T0076, NNX17AI50G, NNX16AQ87G., 80NSSC19K0270, 80NSSC19K0843, 80NSSC18K0835, 80NSSC20K0355, NNX17AI47G, 80NSSC20K0704, 80NSSC18K1578]

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The Kelvin-Helmholtz instability of magnetohydrodynamic surface waves at the low latitude boundary layer is examined using both an eigenfrequency analysis and a time-dependent wave simulation. The results show the occurrence of unstable KH waves under certain conditions, and the coupling between the secondary KH waves and resonant surface Alfven waves driven by the sheared flow. There are notable differences between the primary and secondary KH waves.
The Kelvin-Helmholtz (KH) instability of magnetohydrodynamic surface waves at the low latitude boundary layer is examined using both an eigenfrequency analysis and a time-dependent wave simulation. The analysis includes the effects of sheared flow and Alfven velocity gradient. When the magnetosheath flows are perpendicular to the ambient magnetic field direction, unstable KH waves that propagate obliquely to the sheared flow direction occur at the sheared flow surface when the Alfven Mach number is higher than an instability threshold. Including a shear transition layer between the magnetosphere and magnetosheath leads to secondary KH waves (driven by the sheared flow) that are coupled to the resonant surface Alfven wave. There are remarkable differences between the primary and the secondary KH waves, including wave frequency, the growth rate, and the ratio between the transverse and compressional components. The secondary KH wave energy is concentrated near the shear Alfven wave frequency at the magnetosheath with a lower frequency than the primary KH waves. Although the growth rate of the secondary KH waves is lower than the primary KH waves, the threshold condition is lower, so it is expected that these types of waves will dominate at a lower Mach number. Because the transverse component of the secondary KH waves is stronger than that of the primary KH waves, more efficient wave energy transfer from the boundary layer to the inner magnetosphere is also predicted.

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