Determine the dominant origin mechanism of magnetic switchbacks
Determine which mechanism—solar-coronal formation through interchange magnetic reconnection or jet-like ejections, or local development through nonlinear Alfvénic turbulence, velocity shear, or large-scale magnetic-field bending—dominates the generation of magnetic switchbacks in the near-Sun solar wind, by connecting in-situ plasma measurements with their coronal source environments.
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The origin of these structures remains a key open question. In the solar-origin scenario, SBs are thought to form near the Sun through processes such as interchange magnetic reconnection or jet-like ejections from open magnetic regions . Recent remote-sensing studies have provided complementary evidence that such reconnection-driven flows in the quiet Sun and coronal holes can give rise to magnetic field kinking and outflows that may evolve into SBs in the nascent solar wind . Alternatively, the in-situ hypothesis suggests that SBs can develop locally as the solar wind expands outward, driven by nonlinear Alfvénic turbulence, velocity shear, or large-scale magnetic-field bending . Determining which of these mechanisms dominates requires detailed case studies that directly connect in-situ plasma measurements with their coronal source environments.