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Author name code: polito
ADS astronomy entries on 2022-09-14
author:Polito, V.

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Title: Diagnostics of non-Maxwellian electron distributions in solar
    active regions from Fe XII lines observed by Hinode/EIS and IRIS
Authors: Del Zanna, G.; Polito, V.; Dudík, J.; Testa, P.; Mason,
   H. E.; Dzifčáková, E.
2022arXiv220707026D    Altcode:
  We present joint Hinode/EIS and IRIS observations of Fe XII lines
  in active regions, both on-disk and off-limb. We use an improved
  calibration for the EIS data, and find that the 192.4 A / 1349 A
  observed ratio is consistent with the values predicted by CHIANTI and
  the coronal approximation in quiescent areas, but not in all active
  region observations, where the ratio is often lower than expected
  by up to a factor of about two. We investigate a number of physical
  mechanisms that could affect this ratio, such as opacity and absorption
  from cooler material. We find significant opacity in the EIS Fe XII
  193 and 195 A lines, but not in the 192.4 A line, in agreement with
  previous findings. As we cannot rule out possible EUV absorption by
  H, He and He II in the on-disk observations, we focus on an off-limb
  observation where such absorption is minimal. After considering these,
  as well as possible non-equilibrium effects, we suggest that the most
  likely explanation for the observed low Fe XII 192.4 A / 1349 A ratio
  is the presence of non-Maxwellian electron distributions in the active
  regions. This is in agreement with previous findings based on EIS and
  IRIS observations independently.

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Title: Blueshifted Si IV 1402.77 Å Line Profiles in a Moving Flare
    Kernel Observed by IRIS
Authors: Lörinčík, Juraj; Dudík, Jaroslav; Polito, Vanessa
2022ApJ...934...80L    Altcode:
  We analyze the spectra of a slipping flare kernel observed during
  the 2015 June 22 M6.5-class flare by the Interface Region Imaging
  Spectrograph (IRIS). During the impulsive and peak phases of the flare,
  loops exhibiting an apparent slipping motion along the ribbons were
  observed in the 131 Å channel of SDO/AIA. The IRIS spectrograph
  slit observed a portion of the ribbons, including a moving kernel
  corresponding to a flare loop footpoint in Si IV, C II, and Mg II at a
  very-high 1 s cadence. The spectra observed in the kernel were mostly
  redshifted and exhibited pronounced red wings, as typically observed
  in large flares. However, in a small region in one of the ribbons, the
  Si IV 1402.77 Å line was partially blueshifted, with the corresponding
  Doppler velocity ∣v <SUB>D</SUB>∣ exceeding 50 km s<SUP>-1</SUP>. In
  the same region, the C II 1334.53, 1335.66, and 1335.71 Å lines were
  weakly blueshifted (∣v <SUB>D</SUB>∣ &lt; 20 km s<SUP>-1</SUP>)
  and showed pronounced blue wings, which were also observed in the Mg
  II k 2796.35 Å as well as the Mg II triplet 2798.75 and 2798.82 Å
  lines. Using high-cadence AIA observations we found that the region
  where the blueshifts occurred corresponds to the accelerating kernel
  front as it moved through a weak field region. The IRIS observations
  with high resolution allowed us to capture the acceleration of the
  kernel under the slit for the first time. The unique observations of
  blueshifted chromospheric and TR lines provide new constraints for
  current models of flares.

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Title: Blueshifted Si IV 1402.77Å line profiles in a moving flare
    kernel observed by IRIS
Authors: Lörinčík, Juraj; Dudík, Jaroslav; Polito, Vanessa
2022arXiv220610114L    Altcode:
  We analyze spectra of a slipping flare kernel observed during the 2015
  June 22 M6.5-class flare by the Interface Region Imaging Spectrograph
  (IRIS). During the impulsive and peak phases of the flare, loops
  exhibiting an apparent slipping motion along the ribbons were observed
  in the 131Å channel of SDO/AIA. The IRIS spectrograph slit observed
  a portion of the ribbons, including a moving kernel corresponding to
  a flare loop footpoint in Si IV, C II, and Mg II at a very-high 1 s
  cadence. The spectra observed in the kernel were mostly redshifted
  and exhibited pronounced red wings, as typically observed in large
  flares. However, in a small region in one of the ribbons, the Si IV
  1402.77Å line was partially blueshifted, with the corresponding Doppler
  velocity |v_{D}| exceeding 50 km s$^{-1}$. In the same region, the C
  II 1334.53Å, 1335.66Å and 1335.71Å lines were weakly blueshifted
  (|v_{D}| &lt; 20 km s$^{-1}$) and showed pronounced blue wings,
  which were observed also in the Mg II k 2796.35Å as well as the
  Mg II triplet 2798.75Å and 2798.82Å lines. Using high-cadence AIA
  observations we found that the region where the blueshifts occurred
  corresponds to the accelerating kernel front as it moved through a
  weak-field region. The IRIS observations with high resolution allowed
  us to capture the acceleration of the kernel under the slit for the
  first time. The unique observations of blueshifted chromospheric and
  TR lines provide new constrains for current models of flares.

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Title: Diagnostics of Non-Maxwellian Electron Distributions in
    Solar Active Regions from Fe XII Lines Observed by the Hinode
    Extreme Ultraviolet Imaging Spectrometer and Interface Region
    Imaging Spectrograph
Authors: Del Zanna, G.; Polito, V.; Dudík, J.; Testa, P.; Mason,
   H. E.; Dzifčáková, E.
2022ApJ...930...61D    Altcode:
  We present joint Hinode Extreme Ultraviolet Imaging Spectrometer
  (EIS) and Interface Region Imaging Spectrograph (IRIS) observations
  of Fe XII lines in active regions, both on-disk and off-limb. We use
  an improved calibration for the EIS data, and find that the 192.4
  Å/1349 Å observed ratio is consistent with the values predicted by
  CHIANTI and the coronal approximation in quiescent areas, but not in
  all active-region observations, where the ratio is often lower than
  expected by up to a factor of about two. We investigate a number of
  physical mechanisms that could affect this ratio, such as opacity and
  absorption from cooler material. We find significant opacity in the EIS
  Fe XII 193 and 195 Å lines, but not in the 192.4 Å line, in agreement
  with previous findings. As we cannot rule out possible EUV absorption by
  H, He, and He II in the on-disk observations, we focus on an off-limb
  observation where such absorption is minimal. After considering these,
  as well as possible nonequilibrium effects, we suggest that the most
  likely explanation for the observed low Fe XII 192.4 Å/1349 Å ratio
  is the presence of non-Maxwellian electron distributions in the active
  regions. This is in agreement with previous findings based on EIS and
  IRIS observations independently.

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Title: Chromospheric emission from nanoflare heating in RADYN
    simulations
Authors: Bakke, H.; Carlsson, M.; Rouppe van der Voort, L.; Gudiksen,
   B. V.; Polito, V.; Testa, P.; De Pontieu, B.
2022A&A...659A.186B    Altcode: 2022arXiv220111961B
  Context. Heating signatures from small-scale magnetic reconnection
  events in the solar atmosphere have proven to be difficult to
  detect through observations. Numerical models that reproduce flaring
  conditions are essential in understanding how nanoflares may act as a
  heating mechanism of the corona. <BR /> Aims: We study the effects of
  non-thermal electrons in synthetic spectra from 1D hydrodynamic RADYN
  simulations of nanoflare heated loops to investigate the diagnostic
  potential of chromospheric emission from small-scale events. <BR />
  Methods: The Mg II h and k, Ca II H and K, Ca II 854.2 nm, and Hα and
  Hβ chromospheric lines were synthesised from various RADYN models of
  coronal loops subject to electron beams of nanoflare energies. The
  contribution function to the line intensity was computed to better
  understand how the atmospheric response to the non-thermal electrons
  affects the formation of spectral lines and the detailed shape of
  their spectral profiles. <BR /> Results: The spectral line signatures
  arising from the electron beams highly depend on the density of the
  loop and the lower cutoff energy of the electrons. Low-energy (5 keV)
  electrons deposit their energy in the corona and transition region,
  producing strong plasma flows that cause both redshifts and blueshifts
  of the chromospheric spectra. Higher-energy (10 and 15 keV) electrons
  deposit their energy in the lower transition region and chromosphere,
  resulting in increased emission from local heating. Our results indicate
  that effects from small-scale events can be observed with ground-based
  telescopes, expanding the list of possible diagnostics for the presence
  and properties of nanoflares.

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Title: Probing the Physics of the Solar Atmosphere with the Multi-slit
    Solar Explorer (MUSE). II. Flares and Eruptions
Authors: Cheung, Mark C. M.; Martínez-Sykora, Juan; Testa, Paola;
   De Pontieu, Bart; Chintzoglou, Georgios; Rempel, Matthias; Polito,
   Vanessa; Kerr, Graham S.; Reeves, Katharine K.; Fletcher, Lyndsay; Jin,
   Meng; Nóbrega-Siverio, Daniel; Danilovic, Sanja; Antolin, Patrick;
   Allred, Joel; Hansteen, Viggo; Ugarte-Urra, Ignacio; DeLuca, Edward;
   Longcope, Dana; Takasao, Shinsuke; DeRosa, Marc L.; Boerner, Paul;
   Jaeggli, Sarah; Nitta, Nariaki V.; Daw, Adrian; Carlsson, Mats; Golub,
   Leon; The
2022ApJ...926...53C    Altcode: 2021arXiv210615591C
  Current state-of-the-art spectrographs cannot resolve the fundamental
  spatial (subarcseconds) and temporal (less than a few tens of
  seconds) scales of the coronal dynamics of solar flares and eruptive
  phenomena. The highest-resolution coronal data to date are based on
  imaging, which is blind to many of the processes that drive coronal
  energetics and dynamics. As shown by the Interface Region Imaging
  Spectrograph for the low solar atmosphere, we need high-resolution
  spectroscopic measurements with simultaneous imaging to understand the
  dominant processes. In this paper: (1) we introduce the Multi-slit Solar
  Explorer (MUSE), a spaceborne observatory to fill this observational
  gap by providing high-cadence (&lt;20 s), subarcsecond-resolution
  spectroscopic rasters over an active region size of the solar transition
  region and corona; (2) using advanced numerical models, we demonstrate
  the unique diagnostic capabilities of MUSE for exploring solar coronal
  dynamics and for constraining and discriminating models of solar flares
  and eruptions; (3) we discuss the key contributions MUSE would make
  in addressing the science objectives of the Next Generation Solar
  Physics Mission (NGSPM), and how MUSE, the high-throughput Extreme
  Ultraviolet Solar Telescope, and the Daniel K Inouye Solar Telescope
  (and other ground-based observatories) can operate as a distributed
  implementation of the NGSPM. This is a companion paper to De Pontieu
  et al., which focuses on investigating coronal heating with MUSE.

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Title: Probing the Physics of the Solar Atmosphere with the Multi-slit
    Solar Explorer (MUSE). I. Coronal Heating
Authors: De Pontieu, Bart; Testa, Paola; Martínez-Sykora, Juan;
   Antolin, Patrick; Karampelas, Konstantinos; Hansteen, Viggo; Rempel,
   Matthias; Cheung, Mark C. M.; Reale, Fabio; Danilovic, Sanja; Pagano,
   Paolo; Polito, Vanessa; De Moortel, Ineke; Nóbrega-Siverio, Daniel;
   Van Doorsselaere, Tom; Petralia, Antonino; Asgari-Targhi, Mahboubeh;
   Boerner, Paul; Carlsson, Mats; Chintzoglou, Georgios; Daw, Adrian;
   DeLuca, Edward; Golub, Leon; Matsumoto, Takuma; Ugarte-Urra, Ignacio;
   McIntosh, Scott W.; the MUSE Team
2022ApJ...926...52D    Altcode: 2021arXiv210615584D
  The Multi-slit Solar Explorer (MUSE) is a proposed mission composed of
  a multislit extreme ultraviolet (EUV) spectrograph (in three spectral
  bands around 171 Å, 284 Å, and 108 Å) and an EUV context imager (in
  two passbands around 195 Å and 304 Å). MUSE will provide unprecedented
  spectral and imaging diagnostics of the solar corona at high spatial
  (≤0.″5) and temporal resolution (down to ~0.5 s for sit-and-stare
  observations), thanks to its innovative multislit design. By obtaining
  spectra in four bright EUV lines (Fe IX 171 Å, Fe XV 284 Å, Fe XIX-Fe
  XXI 108 Å) covering a wide range of transition regions and coronal
  temperatures along 37 slits simultaneously, MUSE will, for the first
  time, "freeze" (at a cadence as short as 10 s) with a spectroscopic
  raster the evolution of the dynamic coronal plasma over a wide range of
  scales: from the spatial scales on which energy is released (≤0.″5)
  to the large-scale (~170″ × 170″) atmospheric response. We use
  numerical modeling to showcase how MUSE will constrain the properties of
  the solar atmosphere on spatiotemporal scales (≤0.″5, ≤20 s) and
  the large field of view on which state-of-the-art models of the physical
  processes that drive coronal heating, flares, and coronal mass ejections
  (CMEs) make distinguishing and testable predictions. We describe the
  synergy between MUSE, the single-slit, high-resolution Solar-C EUVST
  spectrograph, and ground-based observatories (DKIST and others), and
  the critical role MUSE plays because of the multiscale nature of the
  physical processes involved. In this first paper, we focus on coronal
  heating mechanisms. An accompanying paper focuses on flares and CMEs.

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Title: Multi-passband Observations of a Solar Flare over the He I
    10830 Å line
Authors: Xu, Yan; Yang, Xu; Kerr, Graham S.; Polito, Vanessa; Sadykov,
   Viacheslav M.; Jing, Ju; Cao, Wenda; Wang, Haimin
2022ApJ...924L..18X    Altcode: 2021arXiv211209949X
  This study presents a C3.0 flare observed by the Big Bear Solar
  Observatory/Goode Solar Telescope (GST) and Interface Region Imaging
  Spectrograph (IRIS) on 2018 May 28 around 17:10 UT. The Near-Infrared
  Imaging Spectropolarimeter of GST was set to spectral imaging mode to
  scan five spectral positions at ±0.8, ±0.4 Å and line center of He I
  10830 Å. At the flare ribbon's leading edge, the line is observed to
  undergo enhanced absorption, while the rest of the ribbon is observed
  to be in emission. When in emission, the contrast compared to the
  preflare ranges from about 30% to nearly 100% at different spectral
  positions. Two types of spectra, "convex" shape with higher intensity at
  line core and "concave" shape with higher emission in the line wings,
  are found at the trailing and peak flaring areas, respectively. On the
  ribbon front, negative contrasts, or enhanced absorption, of about
  ~10%-20% appear in all five wavelengths. This observation strongly
  suggests that the negative flares observed in He I 10830 Å with
  mono-filtergram previously were not caused by pure Doppler shifts of
  this spectral line. Instead, the enhanced absorption appears to be a
  consequence of flare-energy injection, namely nonthermal collisional
  ionization of helium caused by the precipitation of high-energy
  electrons, as found in our recent numerical modeling results. In
  addition, though not strictly simultaneous, observations of Mg II
  from the IRIS spacecraft, show an obvious central reversal pattern
  at the locations where enhanced absorption of He I 10830 Å is seen,
  which is consistent with previous observations.

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Title: The origin of underdense plasma downflows associated with
    magnetic reconnection in solar flares
Authors: Shen, Chengcai; Chen, Bin; Reeves, Katharine K.; Yu, Sijie;
   Polito, Vanessa; Xie, Xiaoyan
2022NatAs...6..317S    Altcode: 2021arXiv211111407S; 2022NatAs.tmp...29S; 2022NatAs.tmp...23S
  Magnetic reconnection is a universal process that powers explosive
  energy-release events such as solar flares, geomagnetic substorms
  and some astrophysical jets. A characteristic feature of magnetic
  reconnection is the production of fast reconnection outflow jets near
  the plasma Alfvén speeds<SUP>1,2</SUP>. In eruptive solar flares,
  dark finger-shaped plasma downflows moving toward the flare arcade
  have been commonly regarded as the principal observational evidence
  for such reconnection-driven outflows<SUP>3,4</SUP>. However, they
  often show a speed much slower than that expected in reconnection
  theories<SUP>5,6</SUP>, challenging the reconnection-driven
  energy-release scenario in standard flare models. Here we present
  a three-dimensional magnetohydrodynamics model of solar flares. By
  comparing the model predictions with the observed plasma downflow
  features, we conclude that these dark downflows are self-organized
  structures formed in a turbulent interface region below the
  flare termination shock where the outflows meet the flare arcade,
  a phenomenon analogous to the formation of similar structures in
  supernova remnants. This interface region hosts a myriad of turbulent
  flows, electron currents and shocks, crucial for flare energy release
  and particle acceleration.

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Title: Probing the Physics of the Solar Atmosphere with the Multi-slit
Solar Explorer (MUSE): II. Flares and Eruptions
Authors: Cheung, Chun Ming Mark; Martinez-Sykora, Juan; Testa, Paola;
   De Pontieu, Bart; Chintzoglou, Georgios; Rempel, Matthias; Polito,
   Vanessa; Kerr, Graham; Reeves, Katharine; Fletcher, Lyndsay; Jin,
   Meng; Nobrega, Daniel; Danilovic, Sanja; Antolin, Patrick; Allred,
   Joel; Hansteen, Viggo; Ugarte-Urra, Ignacio; DeLuca, Edward; Longcope,
   Dana; Takasao, Shinsuke; DeRosa, Marc; Boerner, Paul; Jaeggli, Sarah;
   Nitta, Nariaki; Daw, Adrian; Carlsson, Mats; Golub, Leon
2021AGUFMSH51A..08C    Altcode:
  Current state-of-the-art spectrographs cannot resolve the fundamental
  spatial (sub-arcseconds) and temporal scales (less than a few tens
  of seconds) of the coronal dynamics of solar flares and eruptive
  phenomena. The highest resolution coronal data to date are based on
  imaging, which is blind to many of the processes that drive coronal
  energetics and dynamics. As shown by IRIS for the low solar atmosphere,
  we need high-resolution spectroscopic measurements with simultaneous
  imaging to understand the dominant processes. In this paper: (1)
  we introduce the Multi-slit Solar Explorer (MUSE), a spaceborne
  observatory to fill this observational gap by providing high-cadence
  (&lt;20 s), sub-arcsecond resolution spectroscopic rasters over an
  active region size of the solar transition region and corona; (2)
  using advanced numerical models, we demonstrate the unique diagnostic
  capabilities of MUSE for exploring solar coronal dynamics, and for
  constraining and discriminating models of solar flares and eruptions;
  (3) we discuss the key contributions MUSE would make in addressing the
  science objectives of the Next Generation Solar Physics Mission (NGSPM),
  and how MUSE, the high-throughput EUV Solar Telescope (EUVST) and the
  Daniel K Inouye Solar Telescope (and other ground-based observatories)
  can operate as a distributed implementation of the NGSPM. This is a
  companion paper to De Pontieu et al. (2021, also submitted to SH-17),
  which focuses on investigating coronal heating with MUSE.

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Title: Spectroscopy of ribbon fronts as diagnostics of energy release
    during solar flares
Authors: Polito, Vanessa; Kerr, Graham; Sadykov, Viacheslav; Xu, Yan
2021AGUFMSH23B..02P    Altcode:
  Lower atmospheric spectra have been observed to show peculiar
  profiles characterized by increased absorption (in He I with GST,
  Xu et al. 2016) as well as broad and reversed profiles (e.g. in Mg
  II and CII with IRIS, Panos et al. 2018, 2021a, 2021b) at the leading
  edge of ribbons during the impulsive phase of flares. In this work, we
  explore the correlation between spectral lines formed across different
  layers of the atmosphere in multiple flares, as observed by IRIS and
  GST. We find that the locations where the increased He I absorption
  or typical broad reverse IRIS chromospheric profiles are observed are
  also regions where transition region and coronal emission as well as
  chromospheric evaporation are weaker. Comparison of these observations
  with predictions from advanced hydrodynamic models provides tight
  constraints into the flare heating models.

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Title: A Novel Integral Field Spectrograph Design for taking
High-Cadence Spectral Solar Images: SNIFS
Authors: Knoer, Vicki; Chamberlin, Phillip; Daw, Adrian; Gong, Qian;
   Milligan, Ryan; Polito, Vanessa; Schmit, Donald
2021AGUFMSH55B1837K    Altcode:
  Many features on the sun such as flares and nanoflares are highly
  dynamic and change over the course of seconds. This is at least an order
  of magnitude faster than our current ability to 2D spectrally image the
  sun. This difference in time scale has made it difficult to study some
  of the sun's faster-changing features. The newly designed Solar eruptioN
  Integral Field Spectrograph (SNIFS) is an extreme ultraviolet (EUV)
  integral field spectrograph which will be able to take spectral images
  of the sun at a 1 second time cadence. The game-changing innovations
  which allow a faster cadence include a fast-readout CMOS detector
  and an array of mirrorlets to focus the incoming light into a square
  array spatial pixels, the spectrum for each of which will be measured
  simultaneously. The optical path is doubled in order to view both active
  network and flaring sun. This new optical design will allow high-cadence
  spectral imaging of the sun which will contribute to our understanding
  of energy and mass transport in the chromosphere and transition region.

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Title: The Formation and Lifetime of Outflows in a Solar Active Region
Authors: Brooks, David H.; Harra, Louise; Bale, Stuart D.; Barczynski,
   Krzysztof; Mandrini, Cristina; Polito, Vanessa; Warren, Harry P.
2021ApJ...917...25B    Altcode: 2021arXiv210603318B
  Active regions are thought to be one contributor to the slow solar
  wind. Upflows in EUV coronal spectral lines are routinely observed at
  their boundaries, and provide the most direct way for upflowing material
  to escape into the heliosphere. The mechanisms that form and drive these
  upflows, however, remain to be fully characterized. It is unclear how
  quickly they form, or how long they exist during their lifetimes. They
  could be initiated low in the atmosphere during magnetic flux emergence,
  or as a response to processes occurring high in the corona when the
  active region is fully developed. On 2019 March 31 a simple bipolar
  active region (AR 12737) emerged and upflows developed on each side. We
  used observations from Hinode, SDO, IRIS, and Parker Solar Probe (PSP)
  to investigate the formation and development of the upflows from the
  eastern side. We used the spectroscopic data to detect the upflow,
  and then used the imaging data to try to trace its signature back to
  earlier in the active region emergence phase. We find that the upflow
  forms quickly, low down in the atmosphere, and that its initiation
  appears associated with a small field-opening eruption and the onset
  of a radio noise storm detected by PSP. We also confirmed that the
  upflows existed for the vast majority of the time the active region
  was observed. These results suggest that the contribution to the solar
  wind occurs even when the region is small, and continues for most of
  its lifetime.

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Title: Observation of bi-directional jets in a prominence
Authors: Hillier, A.; Polito, V.
2021A&A...651A..60H    Altcode:
  Quiescent prominences host a large range of flows, many driven
  by buoyancy, which lead to velocity shear. The presence of these
  shear flows could bend and stretch the magnetic field resulting
  in the formation of current sheets which can lead to magnetic
  reconnection. Though this has been hypothesised to occur in
  prominences, with some observations that are suggestive of
  this process, clear evidence has been lacking. In this paper
  we present observations performed on June 30, 2015 using the
  Interface Region Imaging Spectrograph Si IV and Mg II slit-jaw
  imagers of two bi-directional jets that occur inside the body of
  the prominence. Such jets are highly consistent with what would be
  expected from magnetic reconnection theory. Using this observation,
  we estimate that the prominence under study has an ambient field
  strength in the range of 4.5−9.2 G with `turbulent' field strengths
  of 1 G. Our results highlight the ability of gravity-driven flows
  to stretch and fold the magnetic field of the prominence, implying
  that locally, the quiescent prominence field can be far from a
  static, force-free magnetic field. <P />Movies are available at <A
  href="https://www.aanda.org/10.1051/0004-6361/201935774/olm">https://www.aanda.org</A>

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Title: The Crucial Role Of Non-thermal Electrons In Solar
    Flare-induced Dimming Of He I 10830
Authors: Kerr, G.; Xu, Y.; Allred, J.; Polito, V.; Sadykov, V.; Huang,
   N.; Wang, H.
2021AAS...23830307K    Altcode:
  While solar flares are predominantly characterised by an intense
  broadband enhancement to the solar radiative output, certain
  spectral lines and continua will, in theory, exhibit flare-induced
  dimmings. Observations of orthohelium spectral transitions (He I 10830Å
  and the He I D3 lines near 5876A) have shown evidence of such dimming
  in some weak flares, usually followed by enhanced emission. It has been
  suggested that the presence of non-thermal collisional ionisation of
  helium by the electron beam, followed by recombinations to orthohelium,
  is responsible for overpopulating the orthohelium levels leading to
  stronger absorption. However it has not been possible observationally
  to preclude the possibility of overpopulating orthohelium via enhanced
  photoionisation of He I by EUV irradiance from the flaring corona
  followed by recombinations. Here we present radiation hydrodynamics
  simulations of non-thermal electron beam-driven flares where (1) both
  non-thermal collisional ionisation of Helium and coronal irradiance
  are included, and (2) only coronal irradiance is included. A grid of
  simulations covering a range of total energies deposited by the electron
  beam, and a range of non-thermal electron beam low-energy cutoff values,
  were simulated. For each simulation the He I 10830A line was forward
  modelled. In order to obtain flare-induced dimming of the He I 10830A
  line it was necessary for non-thermal collisional ionisations to be
  present. Further, the effect was more prominent in flares with harder
  non-thermal electron spectrum (larger low-energy cutoff values) and
  longer lived in weaker flares and flares with a more gradual energy
  deposition timescale. These results demonstrate the usefulness of
  orthohelium line emission as a diagnostic of flare energy transport.

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Title: Multi-passband Observations Of A Negative Flare Near He I
    10830 Å
Authors: Xu, Y.; Yang, X.; Kerr, G.; Polito, V.; Jing, J.; Cao, W.;
   Wang, H.
2021AAS...23830305X    Altcode:
  This study presents a C3.0 flare observed by the BBSO/GST and
  IRIS, on 2018-May-28 around 17:10 UT. The Near Infrared Imaging
  Spectropolarimeter (NIRIS) was set to spectral imaging mode to scan
  five spectral positions at ±0.8 Å, ±0.4 Å and line center of He I
  10830 Å. Negative contrasts of around 10%, appear in all of the five
  wavelengths, with a weak dependence of these wavelengths. This means
  that the line is undergoing enhanced absorption at these times. The
  observations confirm that the negative flares observed in He I 10830 Å
  with mono-filtergram previously were not caused by pure Doppler shifts
  of this spectral line. Instead, the enhanced absorption is a consequence
  of nonthermal ionization of helium following precipitation of high
  energy electrons, as found in recent numerical modeling results. In
  addition, though not strictly simultaneously, the IRIS observations show
  clear central reversals in Mg II lines and strong Doppler shifts in C
  II and Mg II lines at the locations where enhanced absorption in He I
  10830 Å is occurring, consistent with previous observations and the
  modeling. In other locations the Mg II profiles appear as single peaked.

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Title: He I 10830 Å Dimming during Solar Flares. I. The Crucial
    Role of Nonthermal Collisional Ionizations
Authors: Kerr, Graham S.; Xu, Yan; Allred, Joel C.; Polito, Vanessa;
   Sadykov, Viacheslav M.; Huang, Nengyi; Wang, Haimin
2021ApJ...912..153K    Altcode: 2021arXiv210316686K
  While solar flares are predominantly characterized by an intense
  broadband enhancement to the solar radiative output, certain
  spectral lines and continua will, in theory, exhibit flare-induced
  dimmings. Observations of transitions of orthohelium He I λλ 10830
  Å and the He I D3 lines have shown evidence of such dimming, usually
  followed by enhanced emission. It has been suggested that nonthermal
  collisional ionization of helium by an electron beam, followed by
  recombinations to orthohelium, is responsible for overpopulating
  those levels, leading to stronger absorption. However, it has not been
  possible observationally to preclude the possibility of overpopulating
  orthohelium via enhanced photoionization of He I by EUV irradiance from
  the flaring corona followed by recombinations. Here we present radiation
  hydrodynamics simulations of nonthermal electron-beam-driven flares
  where (1) both nonthermal collisional ionization of helium and coronal
  irradiance are included, and (2) only coronal irradiance is included. A
  grid of simulations covering a range of total energies deposited by
  the electron beam and a range of nonthermal electron-beam low-energy
  cutoff values were simulated. In order to obtain flare-induced dimming
  of the He I 10830 Å line, it was necessary for nonthermal collisional
  ionization to be present. The effect was more prominent in flares with
  larger low-energy cutoff values and longer lived in weaker flares and
  flares with a more gradual energy deposition timescale. These results
  demonstrate the usefulness of orthohelium line emission as a diagnostic
  of flare energy transport.

---------------------------------------------------------
Title: A New View of the Solar Interface Region from the Interface
    Region Imaging Spectrograph (IRIS)
Authors: De Pontieu, Bart; Polito, Vanessa; Hansteen, Viggo; Testa,
   Paola; Reeves, Katharine K.; Antolin, Patrick; Nóbrega-Siverio,
   Daniel Elias; Kowalski, Adam F.; Martinez-Sykora, Juan; Carlsson,
   Mats; McIntosh, Scott W.; Liu, Wei; Daw, Adrian; Kankelborg, Charles C.
2021SoPh..296...84D    Altcode: 2021arXiv210316109D
  The Interface Region Imaging Spectrograph (IRIS) has been obtaining
  near- and far-ultraviolet images and spectra of the solar atmosphere
  since July 2013. IRIS is the highest resolution observatory to provide
  seamless coverage of spectra and images from the photosphere into the
  low corona. The unique combination of near- and far-ultraviolet spectra
  and images at sub-arcsecond resolution and high cadence allows the
  tracing of mass and energy through the critical interface between the
  surface and the corona or solar wind. IRIS has enabled research into the
  fundamental physical processes thought to play a role in the low solar
  atmosphere such as ion-neutral interactions, magnetic reconnection, the
  generation, propagation, and dissipation of waves, the acceleration of
  non-thermal particles, and various small-scale instabilities. IRIS has
  provided insights into a wide range of phenomena including the discovery
  of non-thermal particles in coronal nano-flares, the formation and
  impact of spicules and other jets, resonant absorption and dissipation
  of Alfvénic waves, energy release and jet-like dynamics associated
  with braiding of magnetic-field lines, the role of turbulence and the
  tearing-mode instability in reconnection, the contribution of waves,
  turbulence, and non-thermal particles in the energy deposition during
  flares and smaller-scale events such as UV bursts, and the role of flux
  ropes and various other mechanisms in triggering and driving CMEs. IRIS
  observations have also been used to elucidate the physical mechanisms
  driving the solar irradiance that impacts Earth's upper atmosphere,
  and the connections between solar and stellar physics. Advances in
  numerical modeling, inversion codes, and machine-learning techniques
  have played a key role. With the advent of exciting new instrumentation
  both on the ground, e.g. the Daniel K. Inouye Solar Telescope (DKIST)
  and the Atacama Large Millimeter/submillimeter Array (ALMA), and
  space-based, e.g. the Parker Solar Probe and the Solar Orbiter, we aim
  to review new insights based on IRIS observations or related modeling,
  and highlight some of the outstanding challenges.

---------------------------------------------------------
Title: Future perspectives in solar hot plasma observations in the
    soft X-rays
Authors: Corso, Alain Jody; Del Zanna, Giulio; Polito, Vanessa
2021ExA...tmp...49C    Altcode: 2021arXiv210505549C
  The soft X-rays (SXRs: 90-150 Å) are among the most interesting
  spectral ranges to be investigated in the next generation of solar
  missions due to their unique capability of diagnosing phenomena
  involving hot plasma with temperatures up to 15 MK. Multilayer
  (ML) coatings are crucial for developing SXR instrumentation, as
  so far they represent the only viable option for the development
  of high-efficiency mirrors in the this spectral range. However, the
  current standard MLs are characterized by a very narrow spectral band
  which is incompatible with the science requirements expected for a SXR
  spectrometer. Nevertheless, recent advancement in the ML technology has
  made the development of non-periodic stacks repeatable and reliable,
  enabling the manufacturing of SXR mirrors with a valuable efficiency
  over a large range of wavelengths. In this work, after reviewing the
  state-of-the-art ML coatings for the SXR range, we investigate the
  possibility of using M-fold and aperiodic stacks for the development
  of multiband SXR spectrometers. After selecting a possible choice
  of key spectral lines, some trade-off studies for an eight-bands
  spectrometer are also presented and discussed, giving an evaluation
  of their feasibility and potential performance.

---------------------------------------------------------
Title: Solar Flare Arcade Modelling using Field-Aligned Flare
Simulations: Bridging the gap from 1D to 3D
Authors: Kerr, G. S.; Allred, J. C.; Polito, V.
2020AGUFMSH0500009K    Altcode:
  Solar flares are 3D phenomenon but modelling a flare in 3D, including
  many of the important processes in the chromosphere, is a computational
  challenge. Accurately modelling the chromosphere is important, even
  if the transition region and corona are the areas of interest, due to
  the flow of energy, mass, and radiation through the interconnected
  layers. We present a solar flare arcade model, that aims to bridge
  the gap between 1D and 3D modelling. Our approach is limited to
  the synthesis of optically thin emission. Using observed active
  region loop structures in a 3D domain we graft simulated 1D flare
  atmospheres onto each loop, synthesise the emission and then project
  that emission onto to the 2D observational plane. Emission from SDO/AIA,
  GOES/XRS, and IRIS/SG Fe XXI 1354.1A was forward modelled. We analyse
  the temperatures, durations, mass flows, and line widths associated
  with the flare, finding qualitative agreement but certain quantitative
  differences. Compared to observations, the Doppler shifts are of similar
  magnitude but decay too quickly. They are not as ordered, containing
  a larger amount of scatter compared to observations. The duration of
  gradual phase emission from GOES and AIA emission is also too short. Fe
  XXI lines are broadened, but not sufficiently. These findings suggest
  that additional physics is required in our model. The arcade model
  that we show here as a proof-of-concept can be extended to investigate
  other lines and global aspects of solar flares, providing a means to
  better test the coronal response to models of flare energy injection.

---------------------------------------------------------
Title: The Solar eruptioN Integral Field Spectrograph (SNIFS)
    Sounding Rocket
Authors: Chamberlin, P. C.; Schmit, D. J.; Daw, A. N.; Polito, V.;
   Gong, Q.; Milligan, R. O.
2020AGUFMSH056..03C    Altcode:
  The lower solar atmosphere is temporally dynamic and spatially
  inhomogeneous, and it is becoming increasingly clear that this
  complex activity must be measured and quantified if we are to fully
  understand how mass and energy are transported into the corona. The
  Solar eruptioN Integral Field Spectrograph (SNIFS) sounding rocket is
  designed to break new ground by using a unique set of capabilities to
  probe the most vexingly complex region of the solar atmosphere, the
  chromosphere. Hydrogen Lyman-alpha (Ly-α; 121.6 nm) is the brightest
  line in the solar UV spectrum, it is energetically one of the most
  important. Using radiation transfer models, we can use the observed line
  profiles to reconstruct the transit of these photon through the solar
  atmosphere and understand the plasma from which they came. SNIFS will
  observe not only Ly-ɑ, but the nearby Si III and O V emissions, two
  transition regions lines that allow us to observe how the chromosphere
  connects with upper atmosphere. The SNIFS rocket mission has a primary
  objective to explore the energetics and dynamics of chromosphere using
  a next-generation solar spectral imager. <P />SNIFS will be the first
  of its kind: a solar ultraviolet integral field spectrograph (IFS;
  Chamberlin and Gong, 2016). SNIFS technology will revolutionize solar
  observations by obtaining high cadence 3D information simultaneously:
  two spatial dimensions and one spectral dimensions.SNIFS utilizes a
  novel optical design to simultaneously observe a 32 x 32 arcsec field
  of view with 0.45 arcsec pixels, with a spectral resolution of 66mÅ
  and at 1 s cadence. The SNIFS design employs, for the first time in
  a spaceflight instrument as a technology development, a 72x72 element
  2D array of reflecting and focusing mirrorlets, allowing IFS concepts
  to move down into EUV wavelengths. This mirrorlet array is placed
  at the imaging plane of the telescope, similar to the location of
  a slit in a traditional imaging slit-spectrometer design. After the
  mirrorlet in the optical path, a focusing grating will then produce
  a high-resolution spectrum for each spatial element defined by the
  mirrorlet elements. SNIFS's IFS technology is truly a game-changing
  instrument needed for future solar physics missions, and was recently
  selected and funded by NASA to fly in Spring of 2024.

---------------------------------------------------------
Title: Hot Plasma Flows and Oscillations in the Loop-top Region
    During the 2017 September 10 X8.2 Solar Flare
Authors: Reeves, Katharine K.; Polito, Vanessa; Chen, Bin; Galan,
   Giselle; Yu, Sijie; Liu, Wei; Li, Gang
2020ApJ...905..165R    Altcode: 2020arXiv201012049R
  In this study, we investigate motions in the hot plasma above the
  flare loops during the 2017 September 10 X8.2 flare event. We examine
  the region to the south of the main flare arcade, where there is data
  from the Interface Region Imaging Spectrograph (IRIS) and the Extreme
  ultraviolet Imaging Spectrometer (EIS) on Hinode. We find that there are
  initial blueshifts of 20-60 km s<SUP>-1</SUP> observed in this region
  in the Fe XXI line in IRIS and the Fe XXIV line in EIS, and that the
  locations of these blueshifts move southward along the arcade over the
  course of about 10 minutes. The cadence of IRIS allows us to follow
  the evolution of these flows, and we find that at each location where
  there is an initial blueshift in the Fe XXI line, there are damped
  oscillations in the Doppler velocity with periods of ∼400 s. We
  conclude that these periods are independent of loop length, ruling
  out magnetoacoustic standing modes as a possible mechanism. Microwave
  observations from the Expanded Owens Valley Solar Array (EOVSA)
  indicate that there are nonthermal emissions in the region where the
  Doppler shifts are observed, indicating that accelerated particles
  are present. We suggest that the flows and oscillations are due to
  motions of the magnetic field that are caused by reconnection outflows
  disturbing the loop-top region.

---------------------------------------------------------
Title: IRIS Observations of the Low-atmosphere Counterparts of Active
    Region Outflows
Authors: Polito, Vanessa; De Pontieu, Bart; Testa, Paola; Brooks,
   David H.; Hansteen, Viggo
2020ApJ...903...68P    Altcode: 2020arXiv201015945P
  Active region (AR) outflows have been studied in detail since
  the launch of Hinode/EIS and are believed to provide a possible
  source of mass and energy to the slow solar wind. In this work, we
  investigate the lower atmospheric counterpart of AR outflows using
  observations from the Interface Region Imaging Spectrograph (IRIS). We
  find that the IRIS Si IV, C II&gt; and Mg II transition region (TR)
  and chromospheric lines exhibit different spectral features in the
  outflows as compared to neighboring regions at the footpoints ("moss")
  of hot AR loops. The average redshift of Si IV in the outflow region
  (≍5.5 km s<SUP>-1</SUP>) is smaller than typical moss (≍12-13
  km s<SUP>-1</SUP>) and quiet Sun (≍7.5 km s<SUP>-1</SUP>) values,
  while the C II line is blueshifted (≍-1.1-1.5 km s<SUP>-1</SUP>),
  in contrast to the moss where it is observed to be redshifted by
  about ≍2.5 km s<SUP>-1</SUP>. Further, we observe that the low
  atmosphere underneath the coronal outflows is highly structured, with
  the presence of blueshifts in Si IV and positive Mg II k2 asymmetries
  (which can be interpreted as signatures of chromospheric upflows)
  which are mostly not observed in the moss. These observations show a
  clear correlation between the coronal outflows and the chromosphere
  and TR underneath, which has not been shown before. Our work strongly
  suggests that these regions are not separate environments and should
  be treated together, and that current leading theories of AR outflows,
  such as the interchange reconnection model, need to take into account
  the dynamics of the low atmosphere.

---------------------------------------------------------
Title: Solar Flare Arcade Modeling: Bridging the Gap from 1D to 3D
    Simulations of Optically Thin Radiation
Authors: Kerr, Graham S.; Allred, Joel C.; Polito, Vanessa
2020ApJ...900...18K    Altcode: 2020arXiv200713856K
  Solar flares are 3D phenomena, but modeling a flare in 3D, including
  many of the important processes in the chromosphere, is a computational
  challenge. Accurately modeling the chromosphere is important, even if
  the transition region and corona are the areas of interest, due to
  the flow of energy, mass, and radiation through the interconnected
  layers. We present a solar flare arcade model that aims to bridge
  the gap between 1D and 3D modeling. Our approach is limited to
  the synthesis of optically thin emission. Using observed active
  region loop structures in a 3D domain, we graft simulated 1D flare
  atmospheres onto each loop, synthesize the emission, and then project
  that emission onto the 2D observational plane. Emission from SDO/AIA,
  GOES/XRS, and IRIS/SG Fe XXI λ1354.1 was forward modeled. We analyze
  the temperatures, durations, mass flows, and line widths associated
  with the flare, finding qualitative agreement but certain quantitative
  differences. Compared to observations, the Doppler shifts are of similar
  magnitude but decay too quickly. They are not as ordered, containing
  a larger amount of scatter compared to observations. The duration of
  gradual phase emission from GOES and AIA emission is also too short. Fe
  XXI lines are broadened, but not sufficiently. These findings suggest
  that additional physics is required in our model. The arcade model
  that we show here as a proof of concept can be extended to investigate
  other lines and global aspects of solar flares, providing a means to
  better test the coronal response to models of flare energy injection.

---------------------------------------------------------
Title: Solar Flare Energy Partitioning and Transport -- the Impulsive
    Phase (a Heliophysics 2050 White Paper)
Authors: Kerr, Graham S.; Alaoui, Meriem; Allred, Joel C.; Bian,
   Nicholas H.; Dennis, Brian R.; Emslie, A. Gordon; Fletcher, Lyndsay;
   Guidoni, Silvina; Hayes, Laura A.; Holman, Gordon D.; Hudson, Hugh
   S.; Karpen, Judith T.; Kowalski, Adam F.; Milligan, Ryan O.; Polito,
   Vanessa; Qiu, Jiong; Ryan, Daniel F.
2020arXiv200908400K    Altcode:
  Solar flares are a fundamental component of solar eruptive events (SEEs;
  along with solar energetic particles, SEPs, and coronal mass ejections,
  CMEs). Flares are the first component of the SEE to impact our
  atmosphere, which can set the stage for the arrival of the associated
  SEPs and CME. Magnetic reconnection drives SEEs by restructuring the
  solar coronal magnetic field, liberating a tremendous amount of energy
  which is partitioned into various physical manifestations: particle
  acceleration, mass and magnetic-field eruption, atmospheric heating,
  and the subsequent emission of radiation as solar flares. To explain
  and ultimately predict these geoeffective events, the heliophysics
  community requires a comprehensive understanding of the processes that
  transform and distribute stored magnetic energy into other forms,
  including the broadband radiative enhancement that characterises
  flares. This white paper, submitted to the Heliophysics 2050 Workshop,
  discusses the flare impulsive phase part of SEEs, setting out the
  questions that need addressing via a combination of theoretical,
  modelling, and observational research. In short, by 2050 we must
  determine the mechanisms of particle acceleration and propagation,
  and must push beyond the paradigm of energy transport via nonthermal
  electron beams, to also account for accelerated protons &amp; ions
  and downward directed Alfven waves.

---------------------------------------------------------
Title: Solar Flare Energy Partitioning and Transport -- the Gradual
    Phase (a Heliophysics 2050 White Paper)
Authors: Kerr, Graham S.; Alaoui, Meriem; Allred, Joel C.; Bian,
   Nicholas H.; Dennis, Brian R.; Emslie, A. Gordon; Fletcher, Lyndsay;
   Guidoni, Silvina; Hayes, Laura A.; Holman, Gordon D.; Hudson, Hugh
   S.; Karpen, Judith T.; Kowalski, Adam F.; Milligan, Ryan O.; Polito,
   Vanessa; Qiu, Jiong; Ryan, Daniel F.
2020arXiv200908407K    Altcode:
  Solar flares are a fundamental component of solar eruptive events
  (SEEs; along with solar energetic particles, SEPs, and coronal
  mass ejections, CMEs). Flares are the first component of the SEE
  to impact our atmosphere, which can set the stage for the arrival
  of the associated SEPs and CME. Magnetic reconnection drives SEEs
  by restructuring the solar coronal magnetic field, liberating a
  tremendous amount of energy which is partitioned into various physical
  manifestations: particle acceleration, mass and magnetic-field eruption,
  atmospheric heating, and the subsequent emission of radiation as solar
  flares. To explain and ultimately predict these geoeffective events,
  the heliophysics community requires a comprehensive understanding of
  the processes that transform and distribute stored magnetic energy
  into other forms, including the broadband radiative enhancement that
  characterises flares. This white paper, submitted to the Heliophysics
  2050 Workshop, discusses the flare gradual phase part of SEEs, setting
  out the questions that need addressing via a combination of theoretical,
  modelling, and observational research. In short, the flare gradual phase
  persists much longer than predicted so, by 2050, we must identify the
  characteristics of the significant energy deposition sustaining the
  gradual phase, and address the fundamental processes of turbulence
  and non-local heat flux.

---------------------------------------------------------
Title: Solar Flare Arcade Modelling: Bridging the gap from 1D to 3D
    Simulations of Optically Thin Radiation
Authors: Kerr, G. S.; Allred, J.; Polito, V.
2020SPD....5121106K    Altcode:
  Solar flares are 3D phenomenon but modelling a flare in 3D, including
  many of the important processes in the chromosphere, is a computational
  challenge. Accurately modelling the chromosphere is important, even
  if the transition region and corona are the areas of interest, due to
  the flow of energy, mass, and radiation through the interconnected
  layers. We present a solar flare arcade model, that aims to bridge
  the gap between 1D and 3D modelling. Our approach is limited to the
  synthesis of optically thin emission. Using observed active region
  loop structures in a 3D domain we graft simulated 1D flare atmospheres
  onto each loop, synthesise the emission and then project that emission
  onto to the 2D observational plane. Emission from SDO/AIA, GOES/XRS,
  and IRIS/SG Fe XXI 1354.1Å was forward modelled. We analyse the
  temperatures, durations, mass flows, and line widths associated with
  the flare, finding qualitative agreement but certain quantitative
  differences. Compared to observations, the Doppler shifts are of similar
  magnitude but decay too quickly. They are not as ordered, containing
  a larger amount of scatter compared to observations. The duration of
  gradual phase emission from GOES and AIA emission is also too short. Fe
  XXI lines are broadened, but not sufficiently. These findings suggest
  that additional physics is required in our model. The arcade model
  that we show here as a proof-of-concept can be extended to investigate
  other lines and global aspects of solar flares, providing a means to
  better test the coronal response to models of flare energy injection.

---------------------------------------------------------
Title: Roadmap on cosmic EUV and x-ray spectroscopy
Authors: Smith, Randall; Hahn, Michael; Raymond, John; Kallman, T.;
   Ballance, C. P.; Polito, Vanessa; Del Zanna, Giulio; Gu, Liyi; Hell,
   Natalie; Cumbee, Renata; Betancourt-Martinez, Gabriele; Costantini,
   Elisa; Corrales, Lia
2020JPhB...53i2001S    Altcode:
  Cosmic EUV/x-ray spectroscopists, including both solar and astrophysical
  analysts, have a wide range of high-resolution and high-sensitivity
  tools in use and a number of new facilities in development for
  launch. As this bandpass requires placing the spectrometer beyond
  the Earth's atmosphere, each mission represents a major investment
  by a national space agency such as NASA, ESA, or JAXA, and more
  typically a collaboration between two or three. In general justifying
  new mission requires an improvement in capabilities of at least an
  order of magnitude, but the sensitivity of these existing missions
  are already taxing existing atomic data quantity and accuracy. This
  roadmap reviews the existing missions, showing how in a number of areas
  atomic data limits the science that can be performed. The missions that
  will be launched in the coming Decade will without doubt require both
  more and improved measurements of wavelengths and rates, along with
  theoretical calculations of collisional and radiative cross sections
  for a wide range of processes.

---------------------------------------------------------
Title: IRIS Observations of Short-term Variability in Moss Associated
    with Transient Hot Coronal Loops
Authors: Testa, Paola; Polito, Vanessa; De Pontieu, Bart
2020ApJ...889..124T    Altcode: 2019arXiv191008201T
  We observed rapid variability (≲60 s) at the footpoints of transient,
  hot (∼8-10 MK) coronal loops in active region cores, with the
  Interface Region Imaging Spectrograph (IRIS). The high spatial (∼0"33)
  and temporal (≲5-10 s) resolution of IRIS is often crucial for the
  detection of this variability. We show how, in combination with 1D RADYN
  loop modeling, these IRIS spectral observations of the transition region
  (TR) and chromosphere provide powerful diagnostics of the properties of
  coronal heating and energy transport (thermal conduction or nonthermal
  electrons, NTEs). Our simulations of nanoflare-heated loops indicate
  that emission in the Mg II triplet can be used as a sensitive diagnostic
  for nonthermal particles. In our events, we observe a large variety
  of IRIS spectral properties (intensity, Doppler shifts, broadening,
  chromospheric/TR line ratios, Mg II triplet emission) even for
  different footpoints of the same coronal events. In several events,
  we find spectroscopic evidence for NTEs (e.g., TR blueshifts and Mg
  II triplet emission), suggesting that particle acceleration can occur
  even for very small magnetic reconnection events, which are generally
  below the detection threshold of hard X-ray instruments that provide
  direct detection of emission of nonthermal particles.

---------------------------------------------------------
Title: Loop-top oscillations observed with IRIS spatially correlated
    with nonthermal emission from EOVSA in the September 10 2017 X8 Flare
Authors: Reeves, K.; Polito, V.; Galan, G.; Yu, S.; Chen, B.; Liu,
   W.; Li, G.
2019AGUFMSH13D3416R    Altcode:
  he September 10 2017 X8 flare was a spectacular limb event complete with
  a fast coronal mass ejection, a fully global EUV wave, a bright flare
  loop arcade, and strong emission ranging from microwave to white-light
  continuum and gamma-rays. We examine the IRIS Fe XXI data from this
  event. Fe XXI is a coronal line that is formed at about 10 MK. The IRIS
  pointing was just south of the main cusp-shaped loop structure visible
  in AIA, but it did capture most of the flare arcade on the limb. We find
  that the majority of the emission in the loops is slightly red shifted,
  with speeds of about 20 km/s, probably due to chromospheric evaporation
  and an inclined viewing angle. During the period from 16:05 - 16:15
  UT, we find that faint blue-shifted regions appear at the top of the
  flare loops, indicating plasma flows of 20-60 km/s. After the initial
  blue shift at each location, the Fe XXI Doppler velocities exhibit a
  damped oscillation with a period of about 40 sec. Interestingly, in
  the minutes before the blue-shifted loop-top emission was observed,
  the Expanded Owens Valley Solar Array observed nonthermal microwave
  emission at the same location above the loop-tops, possibly indicative
  of particle acceleration there. We will discuss possible mechanisms
  for these observations.

---------------------------------------------------------
Title: Diagnostics of nanoflare heating in active region core loops
    from chromospheric and transition region observations and modeling
Authors: Testa, P.; Polito, V.; De Pontieu, B.; Reale, F.; Graham, D.
2019AGUFMSH13B..07T    Altcode:
  Rapid variability at the footpoints of active region coronal loops
  has been observed (Testa et al. 2013, 2014), and provides powerful
  diagnostics of the properties of coronal heating and energy transport
  (e.g., Testa et al. 2014, Polito et al. 2018, Reale et al. 2019, Testa
  et al. 2019). <P />We will present results of our detailed analysis of
  a dozen of IRIS/AIA observations of footpoints brightenings associated
  with coronal heating, and will present the distribution of the observed
  properties (e.g., duration of brightenings, intensity ratios, Doppler
  shifts, non-thermal broadening,..). We will discuss the properties
  of coronal heating as inferred from the coupling of these high
  spatial, spectral, and temporal resolution chromospheric/transition
  region/coronal observations, with modeling. <P />We will also
  present results of a new algorithm we have developed for an automatic
  detection of these footpoint brightenings in AIA observations (Graham
  et al. 2019), which will allow us, in our next step, to significantly
  expand the number of events detected, and build more robust statistics
  of the properties of nanoflares in active region loops.

---------------------------------------------------------
Title: Can superposition of evaporative flows explain broad IRIS Fe
    XXI line profiles during flares?
Authors: Polito, V.; Testa, P.; De Pontieu, B.
2019AGUFMSH44A..07P    Altcode:
  The observation of the high-temperature (&gt;10MK) IRIS Fe XXI 1354A
  line with the Interface Region Imaging Spectrograph (IRIS) has provided
  significant insights into the chromospheric evaporation process in
  flares. In particular, the line is often observed to be completely
  blueshifted, in contrast to previous observations at lower spatial
  and spectral resolution, and in agreement with predictions from
  theoretical models. Interestingly, the line is also observed to be
  mostly symmetric and significantly broader than expected from thermal
  motions (assuming the peak formation temperature of the ion is in
  equilibrium). One popular interpretation for the non-thermal broadening
  is the superposition of flows from different loop strands. In this work,
  we test this scenario by forward-modelling the Fe XXI line profile
  assuming different possible observational scenarios using hydrodynamic
  simulations of multi-thread flare loops with the 1D RADYN code. Our
  results indicate that the superposition of flows alone cannot easily
  reproduce both the symmetry and the significant broadening of the line
  and that some other physical process, such as turbulence, or a much
  larger ion temperature than previously expected, likely needs to be
  invoked in order to explain the observed profiles.

---------------------------------------------------------
Title: Can the Superposition of Evaporative Flows Explain Broad Fe
    XXI Profiles during Solar Flares?
Authors: Polito, Vanessa; Testa, Paola; De Pontieu, Bart
2019ApJ...879L..17P    Altcode:
  The observation of the high-temperature (≳10 MK) Fe XXI 1354.1
  Å line with the Interface Region Imaging Spectrograph has provided
  significant insights into the chromospheric evaporation process in
  flares. In particular, the line is often observed to be completely
  blueshifted, in contrast to previous observations at lower spatial
  and spectral resolution, and in agreement with predictions from
  theoretical models. Interestingly, the line is also observed to be
  mostly symmetric and significantly broader than expected from thermal
  motions (assuming the peak formation temperature of the ion is in
  equilibrium). One popular interpretation for the nonthermal broadening
  is the superposition of flows from different loop strands. In this
  work, we test this scenario by forward-modeling the Fe XXI line profile
  assuming different possible observational scenarios using hydrodynamic
  simulations of multi-thread flare loops with the 1D RADYN code. Our
  results indicate that the superposition of flows alone cannot easily
  reproduce both the symmetry and the significant broadening of the line
  and that some other physical process, such as turbulence, or a much
  larger ion temperature than previously expected, likely needs to be
  invoked in order to explain the observed profiles.

---------------------------------------------------------
Title: Possible Signatures of a Termination Shock in the 2014 March
    29 X-class Flare Observed by IRIS
Authors: Polito, Vanessa; Galan, Giselle; Reeves, Katharine K.;
   Musset, Sophie
2018ApJ...865..161P    Altcode:
  The standard model of flares predicts the existence of a fast-mode
  magnetohydrodynamic shock above the looptops, also known as termination
  shock (TS), as the result of the downward-directed outflow reconnection
  jets colliding with the closed magnetic loops. A crucial spectral
  signature of a TS is the presence of large Doppler shifts in the spectra
  of high-temperature lines (≥10 MK), which has been rarely observed
  so far. Using high-resolution observations of the Fe XXI line with the
  Interface Region Imaging Spectrograph (IRIS), we detect large redshifts
  (≈200 km s<SUP>-1</SUP>) at the top of the bright looptop arcade of
  the X1-class flare on 2014 March 29. In some cases, the redshifts are
  accompanied by faint simultaneous Fe XXI blueshifts of about -250 km
  s<SUP>-1</SUP>. The values of red and blueshifts are in agreement with
  recent modeling of Fe XXI spectra downflow of the reconnection site and
  previous spectroscopic observations with higher temperature lines. The
  locations where we observe the Fe XXI shifts are co-spatial with 30-70
  keV hard X-ray sources detected by the Reuven Ramaty High Energy Solar
  Spectroscopic Imager (RHESSI), indicating that nonthermal electrons
  are located above the flare loops. We speculate that our results are
  consistent with the presence of a TS in flare reconnection models.

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Title: Broad Non-Gaussian Fe XXIV Line Profiles in the Impulsive
    Phase of the 2017 September 10 X8.3-class Flare Observed by Hinode/EIS
Authors: Polito, Vanessa; Dudík, Jaroslav; Kašparová, Jana;
   Dzifčáková, Elena; Reeves, Katharine K.; Testa, Paola; Chen, Bin
2018ApJ...864...63P    Altcode: 2018arXiv180709361P
  We analyze the spectra of high-temperature Fe XXIV lines observed by
  the Hinode/Extreme-Ultraviolet Imaging Spectrometer (EIS) during the
  impulsive phase of the X8.3-class flare on 2017 September 10. The
  line profiles are broad, show pronounced wings, and clearly depart
  from a single-Gaussian shape. The lines can be well fitted with κ
  distributions, with values of κ varying between ≈1.7 and 3. The
  regions where we observe the non-Gaussian profiles coincide with
  the location of high-energy (≈100-300 keV) hard X-ray (HXR) sources
  observed by RHESSI, suggesting the presence of particle acceleration or
  turbulence, also confirmed by the observations of nonthermal microwave
  sources with the Expanded Owens Valley Solar Array at and above the HXR
  loop-top source. We also investigate the effect of taking into account
  κ distributions in the temperature diagnostics based on the ratio of
  the Fe XXIII λ263.76 and Fe XXIV λ255.1 EIS lines. We found that
  these lines can be formed at much higher temperatures than expected
  (up to log(T[K]) ≈ 7.8) if departures from Maxwellian distributions
  are taken into account. Although larger line widths are expected because
  of these higher formation temperatures, the observed line widths still
  imply nonthermal broadening in excess of 200 km s<SUP>-1</SUP>. The
  nonthermal broadening related to HXR emission is better interpreted
  by turbulence than by chromospheric evaporation.

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Title: Observations of the Kelvin-Helmholtz Instability Driven by
    Dynamic Motions in a Solar Prominence
Authors: Hillier, Andrew; Polito, Vanessa
2018ApJ...864L..10H    Altcode: 2018arXiv180802286H
  Prominences are incredibly dynamic across the whole range of their
  observable spatial scales, with observations revealing gravity-driven
  fluid instabilities, waves, and turbulence. With all of these complex
  motions, it would be expected that instabilities driven by shear in
  the internal fluid motions would develop. However, evidence of these
  have been lacking. Here we present the discovery in a prominence,
  using observations from the Interface Region Imaging Spectrograph,
  of a shear flow instability, the Kelvin-Helmholtz sinusoidal-mode of
  a fluid channel, driven by flows in the prominence body. This finding
  presents a new mechanism through which we can create turbulent motions
  from the flows observed in quiescent prominences. The observation of
  this instability in a prominence highlights their great value as a
  laboratory for understanding the complex interplay between magnetic
  fields and fluid flows that play a crucial role in a vast range of
  astrophysical systems.

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Title: Microwave Spectral Imaging of Bi-Directional Magnetic
    Reconnection Outflow Region of the 2017 Sep 10 X8.2 Flare
Authors: Chen, Bin; Gary, Dale E.; Fleishman, Gregory D.; Krucker,
   Sam; Nita, Gelu M.; Dennis, Brian R.; Yu, Sijie; Kuroda, Natsuha;
   Reeves, Katharine K.; Polito, Vanessa; Shih, Albert
2018shin.confE.211C    Altcode:
  The newly commissioned Expanded Owens Valley Solar Array (EOVSA)
  obtained microwave spectral imaging of the spectacular eruptive solar
  flare on 2017 September 10 in 2.5-18 GHz. During the early impulsive
  phase of the flare ( 15:54 UT), An elongated microwave source appears
  to connect the top of the flare arcade to the bottom of the erupting
  magnetic flux rope. Multi-frequency images reveal that the source
  bifurcates into two parts: One is located at and above the hard X-ray
  looptop source, and another located behind the flux rope. They appear to
  follow closely with the bi-directional reconnection downflow and upflow
  region as inferred from the SDO/AIA EUV images. The spatially resolved
  spectra of this microwave source show characteristics of gyrosynchrotron
  radiation, suggesting the presence of high-energy (100s of keV to MeV)
  electrons throughout the bi-directional reconnection outflow region. We
  derive physical parameters of the source region, and discuss their
  implications in magnetic energy release and electron acceleration.

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Title: Observations of a shear-flow instability driven by dynamic
    prominence motions
Authors: Hillier, Andrew; Polito, . V.
2018cosp...42E1460H    Altcode:
  Prominences are incredibly dynamic across the whole range of their
  observable spatial scales, with observations revealing gravity-driven
  fluid instabilities, waves, and turbulence. With all these complex
  motions, it would be expected that instabilities driven by shear in the
  fluid motions contained in the prominence body would develop. However,
  evidence of these have been lacking. Here we present the discovery in
  a prominence, using observations from the Interface Region Imaging
  Spectrograph (IRIS), of a shear flow instability, a mode of the
  Kelvin-Helmholtz instability that makes streams of fluid develop
  serpentine patterns, driven by transonic motions in the prominence
  body. This finding presents a new mechanism through which we can
  create turbulence from the flows observed in quiescent prominences. The
  observation of this instability in a prominence highlights their great
  value as a laboratory for understanding the complex interplay between
  magnetic fields and fluid flows that play a crucial role in a vast
  range of astrophysical systems.