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Heating of the solar chromosphere through current dissipation
Stockholm University, Faculty of Science, Department of Astronomy. National Solar Observatory, USA.ORCID iD: 0000-0002-3009-295x
Stockholm University, Faculty of Science, Department of Astronomy.ORCID iD: 0000-0002-2344-3993
Stockholm University, Faculty of Science, Department of Astronomy.ORCID iD: 0000-0003-4936-4211
Stockholm University, Faculty of Science, Department of Astronomy.ORCID iD: 0000-0002-4640-5658
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Number of Authors: 82022 (English)In: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 661, article id A59Article in journal (Refereed) Published
Abstract [en]

Context. The solar chromosphere is heated to temperatures higher than predicted by radiative equilibrium. This excess heating is greater in active regions where the magnetic field is stronger.

Aims. We aim to investigate the magnetic topology associated with an area of enhanced millimeter (mm) brightness temperatures in a solar active region mapped by the Atacama Large Millimeter/submillimeter Array (ALMA) using spectropolarimetric co-observations with the 1-m Swedish Solar Telescope (SST).

Methods. We used Milne–Eddington inversions, nonlocal thermodynamic equilibrium (non-LTE) inversions, and a magnetohydrostatic extrapolation to obtain constraints on the three-dimensional (3D) stratification of temperature, magnetic field, and radiative energy losses. We compared the observations to a snapshot of a magnetohydrodynamics simulation and investigate the formation of the thermal continuum at 3 mm using contribution functions.

Results. We find enhanced heating rates in the upper chromosphere of up to ∼5 kW m−2, where small-scale emerging loops interact with the overlying magnetic canopy leading to current sheets as shown by the magnetic field extrapolation. Our estimates are about a factor of two higher than canonical values, but they are limited by the ALMA spatial resolution (∼1.2″). Band 3 brightness temperatures reach about ∼104 K in the region, and the transverse magnetic field strength inferred from the non-LTE inversions is on the order of ∼500 G in the chromosphere.

Conclusions. We are able to quantitatively reproduce many of the observed features including the integrated radiative losses in our numerical simulation. We conclude that the heating is caused by dissipation in current sheets. However, the simulation shows a complex stratification in the flux emergence region where distinct layers may contribute significantly to the emission in the mm continuum.

Place, publisher, year, edition, pages
2022. Vol. 661, article id A59
Keywords [en]
Sun: atmosphere, Sun: chromosphere, Sun: radio radiation, Sun: magnetic fields, Sun: activity
National Category
Astronomy, Astrophysics and Cosmology
Identifiers
URN: urn:nbn:se:su:diva-204698DOI: 10.1051/0004-6361/202243191ISI: 000789980900003OAI: oai:DiVA.org:su-204698DiVA, id: diva2:1658903
Available from: 2022-05-18 Created: 2022-05-18 Last updated: 2022-05-18Bibliographically approved

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da Silva Santos, João ManuelDanilovic, SanjaLeenaarts, Jorritde la Cruz Rodríguez, JaimeVissers, Gregal J. M.

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