@Article{SilvaSCSCWWBV:2022:GeAlMo,
author = "Silva, Jos{\'e} Alexandre de Oliveira e and Selhorst, Caius
Lucius and Costa, Joaquim Eduardo Rezende and Sim{\~o}es, Paulo
J. A. and Castro, Carlos Guillermo Gimenez de and Wedemeyer, Sven
and White, Stephen M. and Brajsa, Roman and Valio, Adriana",
affiliation = "{Universidade de S{\~a}o Paulo (USP)} and {Universidade de
S{\~a}o Paulo (USP)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade Presbiteriana Mackenzie} and
{Universidade Presbiteriana Mackenzie} and {University of Oslo}
and {Air Force Research Laboratory} and {University of Zagreb} and
{Universidade Presbiteriana Mackenzie}",
title = "A Genetic Algorithm to Model Solar Radio Active Regions From 3D
Magnetic Field Extrapolations",
journal = "Frontiers in Astronomy and Space Sciences",
year = "2022",
volume = "9",
pages = "e911118",
month = "June",
keywords = "Sun, radio radiation, atmosphere, magnetic fields, force-free
field extrapolation, Sun-active regions.",
abstract = "In recent decades our understanding of solar active regions (ARs)
has improved substantially due to observations made with better
angular resolution and wider spectral coverage. While prior AR
observations have shown that these structures were always brighter
than the quiet Sun at centimeter wavelengths, recent observations
at millimeter and submillimeter wavelengths have shown ARs with
well defined dark umbrae. Given this new information, it is now
necessary to update our understanding and models of the solar
atmosphere in active regions. In this work, we present a
data-constrained model of the AR solar atmosphere, in which we use
brightness temperature measurements of NOAA 12470 at three radio
frequencies: 17, 100 and 230 GHz. The observations at 17 GHz were
made by the Nobeyama Radioheliograph (NoRH), while the
observations at 100 and 230 GHz were obtained by the Atacama Large
Millimeter/submillimeter Array (ALMA). Based on our model, which
assumes that the radio emission originates from thermal free-free
and gyroresonance processes, we calculate radio brightness
temperature maps that can be compared with the observations. The
magnetic field at distinct atmospheric heights was determined in
our modelling process by force-free field extrapolation using
photospheric magnetograms taken by the Helioseismic and Magnetic
Imager (HMI) on board the Solar Dynamics Observatory (SDO). In
order to determine the best plasma temperature and density height
profiles necessary to match the observations, the model uses a
genetic algorithm that modifies a standard quiet Sun atmospheric
model. Our results show that the height of the transition region
(TR) of the modelled atmosphere varies with the type of region
being modelled: for umbrae the TR is located at 1080 +/- 20 km
above the solar surface; for penumbrae, the TR is located at 1800
+/- 50 km; and for bright regions outside sunspots, the TR is
located at 2000 +/- 100 km. With these results, we find good
agreement with the observed AR brightness temperature maps. Our
modelled AR can be used to estimate the emission at frequencies
without observational coverage.",
doi = "10.3389/fspas.2022.911118",
url = "http://dx.doi.org/10.3389/fspas.2022.911118",
issn = "2296-987X",
language = "en",
targetfile = "fspas-09-911118.pdf",
urlaccessdate = "07 maio 2024"
}