THEMIS Explores the Earth's Bow Shock

  • Released Tuesday, December 11, 2007
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The solar wind's first contact with the Earth's magnetic field creates a region known as the bow shock, much like the bow wave of a boat moving through the water. This region can also create additional turbulence which generates bursts of explosion-like currents. In this visualization, the orbits of the THEMIS fleet are combined with a 2-D slice from a hybrid magnetosphere simulation which illustrates these turbulent regions in the bow shock. This hybrid magnetosphere simulation treats the slow-moving ions by particle-in-cell computational methods and the faster electrons as a massless fluid. These simulations more accurately represent the magnetospheric physics, enabling a view of turbulent non-linear processes not visible in the simpler magnetohydrodynamic models. In this simulation, the color table is somewhat unusual. In order of increasing density, the colors run from white through violet, blue, green to black.

Push in to a view of the satellites in the turbulent region near the bow shock.  The 'bubbles' of violet and white surrounded by green and black illustrate broad the range of particle densities in this turbulence.

Push in to a view of the satellites in the turbulent region near the bow shock. The 'bubbles' of violet and white surrounded by green and black illustrate broad the range of particle densities in this turbulence.

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Credits

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NASA/Goddard Space Flight Center Scientific Visualization Studio

Release date

This page was originally published on Tuesday, December 11, 2007.
This page was last updated on Wednesday, May 3, 2023 at 1:55 PM EDT.


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Related papers

Omidi, N., 'Formation of cavities in the foreshock' in 'Turbulence and nonlinear processes in astrophysical plasmas'. Editors D. Shaikh and G. Zank. AIP Conference Proceedings 932, 2007.

Omidi, N., 'Formation of cavities in the foreshock' in 'Turbulence and nonlinear processes in astrophysical plasmas'. Editors D. Shaikh and G. Zank. AIP Conference Proceedings 932, 2007.


Datasets used

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