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Updated: Jun 6, 2025

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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
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A Novel Determination of the Foreshock ULF Boundary: Statistical Approach
A Salohub1, J Šafránková1, Z Němeček1
1Faculty of Mathematics and Physics Charles University Prague Czech Republic.
Summary
The foreshock wave region
Area of Science:
- Space Physics
- Plasma Physics
- Astrophysics
Background:
- Foreshock waves are crucial for understanding space plasma dynamics.
- Interplanetary Magnetic Field (IMF) orientation influences foreshock wave characteristics.
- Previous studies have indicated a dependence of wave activity on solar wind conditions.
Purpose of the Study:
- To systematically investigate the spatial extent and location of Ultra-low Frequency (ULF) foreshock waves.
- To statistically analyze wave activity in relation to solar wind parameters and IMF orientation.
- To define and utilize a foreshock coordinate system for improved characterization.
Main Methods:
- Statistical analysis of THEMIS mission data.
- Quantification of wave activity using standard deviations of IMF magnitude and components.
- Application of a foreshock coordinate system based on bow shock normal and upstream magnetic field vectors.
- Analysis of wave activity as a function of solar wind bulk speed and Mach number.
Main Results:
- The Ultra-low Frequency (ULF) foreshock boundary is well-defined in the applied coordinate system.
- The foreshock boundary shifts outward with increasing solar wind bulk speed and Mach number.
- Increasing solar wind bulk speed enhances wave activity near the bow shock, while increasing Mach number intensifies it at the foreshock boundary.
Conclusions:
- The spatial extent of foreshock waves is strongly dependent on IMF orientation and solar wind conditions.
- The foreshock coordinate system provides a robust framework for studying wave phenomena.
- Solar wind bulk speed and Mach number have distinct effects on ULF wave activity within the foreshock region.
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