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Resolve the persistent underestimation of heliospheric magnetic field magnitudes in global MHD models

Determine the physical and/or numerical causes of the systematically low magnetic field amplitudes predicted by global heliospheric magnetohydrodynamic models (e.g., MAS with Wave-Turbulence-Driven heating) relative to in-situ observations at 1 AU, and develop validated model improvements that eliminate this discrepancy.

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Background

In the direct comparison for CR2063, the authors note that while many plasma parameters are reasonably captured, the modeled magnetic field strengths remain too low compared to observations.

They emphasize that this is not an isolated issue of the present setup but a broader modeling shortfall reported previously in global heliospheric simulations, citing prior studies that documented the problem. The statement flags the issue as unresolved despite earlier investigations, underscoring a need to identify root causes and corrective strategies.

References

Finally, the lower amplitudes in the modeled field values are a well-known (but, as yet, unresolved) issue with global heliospheric models \citep{linker17a,2019ApJ...884...18R}.

Ion Charge States from a Global Time-Dependent Wave-Turbulence-Driven Model of the Solar Wind: Comparison with in-situ Measurements (2501.04868 - Riley et al., 8 Jan 2025) in Section 3.3 (Comparative Analysis), paragraph discussing the CR2063 direct comparison (after Figure “SimData_CR2063.pdf”)