The Formation of Solar Prominences: Plasma Origin and Mechanisms
Yuhao Zhou
TL;DR
This review addresses how cool, dense prominence plasma originates and is sustained in the hot solar corona. It surveys four mass-accumulation pathways—injection, levitation, evaporation--condensation, and in-situ condensation—grounding each in theory, simulations, and observations, and highlighting the evaporation--condensation route as particularly developed in the past decade. The paper emphasizes that prominences emerge from dynamic magnetic structures and that multiple mechanisms likely operate in concert, with type-dependent dominance (e.g., active regions favoring injection, quiescent filaments favoring condensation). Numerical modeling, from 1D to fully 3D MHD with partial ionization and advanced conduction treatments, reveals coherent mass-loading cycles, thread-like morphologies, and mass–field coupling that reproduce many observed features. The work outlines open questions and calls for integrated multi-scale modeling and high-resolution, multi-wavelength observations to constrain heating, mass budgets, and the coexistence of formation pathways, informing space-weather relevance and solar-terrestrial connections.
Abstract
Solar prominences, or solar filaments, are cool and dense plasma structures in the hot solar corona, whose formation mechanisms have remained a fundamental challenge in solar physics. This review provides a comprehensive overview of the current theoretical, numerical, and observational understanding of prominence formation, with a focus on the origin of the dense plasma component. We begin by summarizing the magnetic field configurations that enable prominence support, followed by a classification of four representative plasma formation mechanisms: injection, levitation, evaporation--condensation, and in-situ condensation. Each mechanism is analyzed in terms of its physical basis, numerical realizations, and observational diagnostics. A central focus is placed on the evaporation--condensation scenario, which has seen significant development over the past decade through numerical simulations. We also discuss recent progress in modeling in-situ condensation triggered by magnetic reconnection and levitation dynamics. Throughout, we emphasize the complementary nature of different mechanisms and their potential coexistence in forming and maintaining prominence mass. Observational constraints and recent high-resolution data are reviewed to assess the physical plausibility of each mechanism. We conclude by highlighting open questions and future directions in connecting multi-scale physical processes to the observed diversity of prominence behaviors.
