Simulations of structured upflows from plumes and their connection to the solar wind
Kamlesh Bora, Lakshmi Pradeep Chitta, Yajie Chen, Damien Przybylski, David Pontin, Nikil Panyam
TL;DR
This work addresses how structured upflows from coronal-hole plumes contribute to the solar wind by examining magnetic topology with 3D radiative MHD simulations. Using the MURaM code, the authors embed a plume into a coronal-hole-like field, synthesize Fe X 174 Å emission, and analyze the interplay between cool lower-atmosphere downflows and hot coronal upflows guided by quasi-separatrix layers (QSLs) at the open-open interface. They find that intense QSL sheets at the OO-interface channel high-velocity, narrow-upflow plumes that persist with height and carry mass flux sufficient to sustain the solar wind, without requiring interchange reconnection at null points. These results suggest a topological pathway for wind acceleration via QSL-mediated reconnection along open flux boundaries, consistent with S-web structures and offering implications for interpreting plume-related EUV signatures from multiple viewing angles.
Abstract
Small-scale transient jetlet activity and associated upflows from coronal hole plumes are potential sources of the solar wind. To elucidate the magnetic origins and driving mechanisms of such upflows, we perform three-dimensional radiative magnetohydrodynamic simulations using the MURaM code, spanning from the upper convection zone to the low corona. We synthesize Fe\,{\sc x} 174\,Å emission to capture the plume evolution comparable to observations, examining underlying plasma flows, thermal structures, and magnetic topologies. We identify a pronounced transition from cool downflows in the lower atmosphere to hot upflows in the corona at the interface between plume-rooted like-polarity flux concentrations. These upflows are threaded by a complex, filamentary network of Quasi-Separatrix Layers (QSLs) -- a topology distinct from standard interchange reconnection scenarios. The domain-averaged mass flux over a 38-minute interval ranges from $10^{-9}$ to $10^{-8}\,\mathrm{g\,cm^{-2}\,s^{-1}}$, substantially exceeding observed solar-wind loss rates. Our results demonstrate that highly structured plasma outflows are channeled along strong QSLs at open--open field boundaries, providing a pathway to sustain the solar wind from coronal-hole plumes without requiring interchange reconnection triggered by opposite-polarity flux emergence.
