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Magneto-Hydrodynamic Equations Mass conservation

Granules in the Quiet and Magnetic Sun Robert F. Stein, Michigan State University Valentyna Abramenko , Big Bear Solar Observatory Åke Nordlund , Niels Bohr Institute, University of Copenhagen. Simulation Results. Magneto-Hydrodynamic Equations Mass conservation

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Magneto-Hydrodynamic Equations Mass conservation

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  1. Granules in the Quiet and Magnetic Sun Robert F. Stein, Michigan State University ValentynaAbramenko, Big Bear Solar Observatory ÅkeNordlund, Niels Bohr Institute, University of Copenhagen Simulation Results Magneto-Hydrodynamic Equations Mass conservation 𝜕𝜌/𝜕t = −∇ · (𝜌u) Momentum conservation𝜕(𝜌u)/𝜕t =−∇·(𝜌uu)−∇𝑃 −𝜌g+J×B−2𝜌Ω×u−∇·𝜏visc Energy conservation𝜕𝑒/𝜕t =−∇·(𝑒u)−𝑃(∇·u)+𝑄rad +𝑄visc +𝜂J2 Induction equation𝜕B/𝜕t = −∇ × E, E=−u×B+𝜂J+ (1/ene) (J×B−∇𝑃e), High resolution simulations and observations reveal that granule properties are very different in quiet Sun and plage regions. In the quiet Sun granules have scalloped edges with turbulent vertical velocity at their edges. In plage granules have swirlingvertical vortex tubes at their edges. Diverging upflowsapproach the downflowintergranular lanes, are deflected by the strong magnetic field and flow around the field creating vertical vortex tubes. The best solar observations currently clearly show the scalloped edges of granules in the quiet Sun intensity images. Small vortex tubes in the intergranular lanes at the edges of strong fields are borderline visible currently. Numerical Method Spatial differencing 6th-order centered finite-differencestaggered Time advancement 3rd order Runga-Kutta Equation of state Tabular including ionization H, He + abundant elements Radiative transfer 3D, LTE 4 bin multi-group Quiet Sun: (left) Vertical velocity image (light is down, gray and dark up) is turbulent at granule edges. (right) Fluid streamlines with volume rendering of magnetic field strength. Horizontal vortex tubes are common, vertical vortex tubes occur at some granule lane vertices. Plasma reaching the surface originates from the centers of underlying larger cells a depth. Rising plasma diverges and turn sover like a fountain and heads back down. Vertical velocity image at continuum optical depth 0.1 with magnetic field contours at 300 & 1000 G. Granule boundaries are corrugated in quiet Sun, but smoother with swirls at boundaries of magentic regions. • Simulation Setup • The computational domain is 2016x500x2016. • It extends 48 Mm wide by20 Mm deep, which is 10% of the geometric depth but 2/3 of the scale heights of the convection zone. • Vertical boundary conditions: Extrapolate lnρ; Velocity -> constant @ top, zero derivative @ bottom; energy/mass -> average value @ top, extrapolate @ bottom; • B tends to potential field @ top, • Inflows at bottom (20 Mm) advect in Weak (1 kG), minimally structured (horizontal, uniform, untwisted) magnetic field . • Initial state – non-magnetic convection. Magnetic Sun: vertical vortex tubes along intergranular lanes. Plasma turning over into intergranular lanes where there are strong magnetic field concentrations wraps around the the magnetic field creating a vertical vortex tube. Continuum intensity image from 12x12x6 Mm simulation, convolved with an 1.5 m airy psf. The scale is not exactly the same as in the observed snapshot. TiOband intensity image from New Solar Telescope (Big Bear Observatory) Granules in field free regions have scalloped edges, whereas in magnetic locations granule boundaries are smoother with swirly strings of bright points. These are bright (as pointed out by HenkSpruit) because where the field is strong, the density is lower and radiation escapes from deeper layers where the plasma gets heated by the deeper hotter walls of the ascending granules. Both the observations with NST and the degraded simulation intensity show a very similar behavior in both the quiet and magnetic locations.

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