trophysical and space weather processes occurs. By virtue of its broad frequency coverage, FASR
will image the entire solar atmosphere multiple times per second from the chromosphere through
the corona, while retaining the capability to image a selected frequency range with as little as 20
ms time resolution. FASR is sensitive to temperatures from <10,000 K to >30 MK, and nonther-
mal particle energies from ∼20 keV to >1MeV. Moreover, FASR’s panoramic view allows the
solar atmosphere and the physical phenomena therein, both thermal and nonthermal, to be studied
as a coupled system.
Here we summarize several main science goals of the proposed instrument while at the same
time emphasizing the fundamentally new observables enabled by FASR. With its unique and inno-
vative capabilities, FASR also has tremendous potential for new discoveries beyond those presently
anticipated.
2.1 The Nature and Evolution of Coronal Magnetic Fields
Quantitative knowledge of coronal magnetic fields is fundamental to understanding essentially
all solar phenomena above the photosphere, including the structure and evolution of solar ac-
tive regions, magnetic energy release, charged particle acceleration, flares, coronal mass ejections
(CMEs), coronal heating, the solar wind and, ultimately, space weather and its impact on Earth.
Characterized as the solar and space physics community’s “dark energy” problem (Lin et al. 2004),
useful quantitative measurements of the coronal magnetic field have been demonstrated with break-
through flare observations by the FASR pathfinder EOVSA (e.g. Gary et al. 2018;Fleishman et al.
2020;Chen et al. 2020b) as well as broadband observations of solar magnetic active regions by
EOVSA and the Jansky Very Large Array (JVLA). Figure 2 illustrates the use of radio observa-
tions for measuring the coronal magnetic field in active regions (ARs). See the white papers by
Gary et al. (2022b) and Chen et al. (2022a) for coronal magnetic field measurements of ARs, coro-
nal cavities, and CMEs. Such measurements are complementary to numerical extrapolations of
the magnetic field distribution at the photospheric or chromospheric level (De Rosa et al. 2009),
as well as ongoing efforts at O/IR wavelengths to make measurements of above-the-limb coronal
magnetic fields via the Hanle and Zeeman effects (e.g., with DKIST and COSMO; see discussion
in Gibson et al. 2021). Coordinating with radio observations (which is already underway with
EOVSA), DKIST and COSMO would enable us to derive the vector magnetic field at the places
where various acceleration and transport mechanisms trigger or operate. The relation between the
inferred vector magnetic field and energy spectra of accelerated particles will strongly constrain
the magnetic reconnection and acceleration mechanisms in transient energy release events such as
flares, CMEs, and jets (e.g. Arnold et al. 2021). See the next subsection for more discussion.
2.2 The Physics of Flares
Outstanding problems in the physics of flares include those of magnetic energy release (Drake
et al. 2014), particle acceleration, and particle transport. As flare energy release requires the par-
ticipation of a large coronal volume sometimes comparable to the size of the entire active region
(Shibata & Magara 2011), one of the key challenges lies in the lack of measurements for key
physical parameters in a broad region around the flare energy release site. At centimeter wave-
lengths, gyrosynchrotron emission – radiation from nonthermal electrons with energies of 10s of
keV to several MeV gyrating in a magnetic field – illuminates any magnetic coronal loop to which
energetic electrons have access, showing when and where accelerated electrons are present. Inver-
sion of the gyrosynchrotron spectrum allows both the magnetic field in the flaring source and the
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