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Updated: Apr 18, 2026

Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
Solution to the cosmic ray anisotropy problem.
Philipp Mertsch1, Stefan Funk1
1Kavli Institute for Particle Astrophysics & Cosmology, 2575 Sand Hill Road, M/S 29, Menlo Park, California 94025, USA.
Cosmic ray (CR) transport models predict a large dipole anisotropy, but observations show a smaller one. This study explains this discrepancy by considering magnetic field variations and CR gradient misalignment, reconciling models with data.
Area of Science:
- Astrophysics
- Cosmic Ray Physics
Background:
- The standard diffusive model for cosmic ray (CR) transport predicts a dipolar anisotropy in their arrival directions.
- This anisotropy is considered a tool for identifying nearby CR sources.
- Observed dipole amplitudes at TeV and PeV energies are significantly smaller than predicted by models.
Purpose of the Study:
- To critically examine the validity of the standard CR transport prediction.
- To investigate the reasons for the discrepancy between predicted and observed dipole amplitudes.
- To reconcile theoretical predictions with observational data.
Main Methods:
- Analyzing deviations of the dipole in specific turbulent magnetic field realizations from ensemble averages.
- Investigating the impact of misalignment between the regular magnetic field and the CR density gradient.
Main Results:
- A significant suppression of the dipole amplitude occurs when the magnetic field and CR gradient directions are nearly perpendicular (∼90°).
- This suppression reconciles the predicted dipole amplitude with observational data.
- The dipole direction generally does not align with the CR gradient direction.
Conclusions:
- The discrepancy between predicted and observed CR dipole anisotropies can be explained by considering specific magnetic field configurations and gradient misalignments.
- The findings resolve a long-standing problem in cosmic ray physics.
- The misalignment between dipole and gradient directions complicates the use of anisotropy as a direct probe for nearby cosmic ray sources.
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