Recent Submissions

  • TOI-2447 b / NGTS-29 b: a 69-day Saturn around a Solar analogue

    Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK; Centre for Exoplanets and Habitability, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK; Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK; Centre for Exoplanets and Habitability, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK;; Observatoire de Genève, Université de Genève, Chemin Pegasi 51, 1290 Versoix, Switzerland; Space Research and Planetary Sciences, Physics Institute, University of Bern, Gesellschaftsstrasse 6, 3012 Bern, Switzerland; Facultad de Ingeniera y Ciencias, Universidad Adolfo Ibáñez, Av. Diagonal las Torres 2640, Peñalolén, Santiago, Chile; Millennium Institute for Astrophysics, Chile; Data Observatory Foundation, Chile; Departamento de Astronomía, Universidad de Chile, Casilla 36-D, Santiago, Chile; Centro de Astrofísica y Tecnologías Afines (CATA), Casilla 36-D, Santiago, Chile;; School of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UK; Carnegie Earth and Planets Laboratory, 5241 Broad Branch Road NW, Washington, DC 20015, USA; Observatoire de Genève, Université de Genève, Chemin Pegasi 51, 1290 Versoix, Switzerland; Mullard Space Science Laboratory, University College London, Holmbury St Mary, Dorking, Surrey, RH5 6NT, UK;; Center for Astrophysics | Harvard;; et al. (Monthly Notices of the Royal Astronomical Society, 2024-08-01)
    Discovering transiting exoplanets with relatively long orbital periods (&gt;10 d) is crucial to facilitate the study of cool exoplanet atmospheres (T<SUB>eq</SUB> &lt; 700 K) and to understand exoplanet formation and inward migration further out than typical transiting exoplanets. In order to discover these longer period transiting exoplanets, long-term photometric, and radial velocity campaigns are required. We report the discovery of TOI-2447 b (=NGTS-29 b), a Saturn-mass transiting exoplanet orbiting a bright (T = 10.0) Solar-type star (T<SUB>eff</SUB> = 5730 K). TOI-2447 b was identified as a transiting exoplanet candidate from a single transit event of 1.3 per cent depth and 7.29 h duration in TESS Sector 31 and a prior transit event from 2017 in NGTS data. Four further transit events were observed with NGTS photometry which revealed an orbital period of P = 69.34 d. The transit events establish a radius for TOI-2447 b of $0.865 \pm 0.010\, \rm R_{\rm J}$, while radial velocity measurements give a mass of $0.386 \pm 0.025\, \rm M_{\rm J}$. The equilibrium temperature of the planet is 414 K, making it much cooler than the majority of TESS planet discoveries. We also detect a transit signal in NGTS data not caused by TOI-2447 b, along with transit timing variations and evidence for a ~150 d signal in radial velocity measurements. It is likely that the system hosts additional planets, but further photometry and radial velocity campaigns will be needed to determine their parameters with confidence. TOI-2447 b/NGTS-29 b joins a small but growing population of cool giants that will provide crucial insights into giant planet composition and formation mechanisms.
  • Decomposing the AIA 304 Å Channel into Its Cool and Hot Components

    Department of Mathematics, Physics and Electrical Engineering, Northumbria University, NE1 8ST, Newcastle upon Tyne, UK; Université Paris-Saclay, CNRS, Institut d'Astrophysique Spatiale, 91405, Orsay, France; Armagh Observatory and Planetarium, BT61 7BH, Armagh, Northern Ireland, UK; Université Paris-Saclay, CNRS, Institut d'Astrophysique Spatiale, 91405, Orsay, France; Institute of Applied Computing and Community Code, Universitat de les Illes Balears, E-07122, Palma de Mallorca, Spain; Institute of Applied Computing and Community Code, Universitat de les Illes Balears, E-07122, Palma de Mallorca, Spain; Institute of Applied Computing and Community Code, Universitat de les Illes Balears, E-07122, Palma de Mallorca, Spain; Departament de Física, Universitat de les Illes Balears, E-07122, Palma de Mallorca, Spain; Antolin, Patrick; Auchère, Frédéric; Winch, Ethan; Soubrié, Elie; Oliver, Ramón (Solar Physics, 2024-07-01)
    The AIA 304 Å channel on board the Solar Dynamics Observatory (SDO) offers a unique view of ≈10<SUP>5</SUP> K plasma emitting in the He II 304 Å line. However, when observing off-limb, the emission of the (small) cool structures in the solar atmosphere (such as spicules, coronal rain and prominence material) can be of the same order as the surrounding hot coronal emission from other spectral lines included in the 304 Å passband, particularly over active regions. In this paper, we investigate three methods based on temperature and morphology that are able to distinguish the cool and hot emission within the 304 Å passband. The methods are based on the Differential Emission Measure (DEM), a linear decomposition of the AIA response functions (RFit) and the Blind Source Separation (BSS) technique. All three methods are found to produce satisfactory results in both quiescent and flaring conditions, largely removing the diffuse corona and leading to images with cool material off-limb in sharp contrast with the background. We compare our results with co-aligned data from the Interface Region Imaging Spectrograph (IRIS) in the SJI 1400 Å and 2796 Å channels, and find the RFit method to best match the quantity and evolution of the cool material detected with IRIS. Some differences can appear due to plasma emitting in the logT =5.1 -5.5 temperature range, particularly during the catastrophic cooling stage prior to rain appearance during flares. These methods are, in principle, applicable to any passband from any instrument suffering from similar cool and hot emission ambiguity, as long as there is good coverage of the high-temperature range.
  • Coma and tail of Comet 67P/Churyumov-Gerasimenko during the 2021-2022 apparition

    Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK; Instituto de Astrofisica de Andalucia, CSIC, Glorieta de la Astronomia s/n, E-18008 Granada, Spain; Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK; Mullard Space Science Laboratory, University College London, Holmbury St. Mary, Dorking RH5 6NT, UK; Boehnhardt, Hermann; Lara, Luisa; Gray, Zuri; Bagnulo, Stefano (Monthly Notices of the Royal Astronomical Society, 2024-07-01)
    We present results on the global activity of comet 67P/Churyumov-Gerasimenko (67P), the ROSETTA target, during its first perihelion passage after the mission and after an encounter with planet Jupiter. 67P was observed by broad-band filter imaging at 33 epochs during 2021 May 21 to 2022 June 1. The mean radial flux profiles suggest that 'equilibrium' conditions for the dust flow in the coma existed from around perihelion until about 100 d thereafter. We propose a scenario for the smaller and larger radial exponents, measured before and after the 'equilibrium' phase. Four coma fans with possible source regions at +40°, -10°, -50°, and -70° latitude on the nucleus are identified. The three fans at southern latitudes may be identical with fan sources seen during post-perihelion in 2015-2016. The rotation axis of 67P may not have changed at all or at least not much (&lt;5°) from the orientation measured during the Rosetta mission at the comet. The dust streamers in the coma originated from observed coma fans, containing mostly dust emitted within days to weeks before observation. Two dust streamers, a long- and a short-lasting one, contained heavy dust grains from emission periods hundreds of days before perihelion. Similar emission periods are obtained for the dust seen in the tail region of the comet. Similarities and differences in the dust activity during the recent apparition with that of the Rosetta mission at the comet are found.
  • Polarimetry of small bodies and satellites of our Solar System

    Armagh Observatory and Planetarium, College Hill, Armagh, UK; Institute of Astronomy, V.N. Karazin Kharkiv National University, Kharkiv, Ukraine; INAF - Osservatorio Astrofisico di Torino, Pino Torinese, Italy; University of Maryland, College Park, MD, USA; Bagnulo, S.; Belskaya, I.; Cellino, A.; Kolokolova, L. (European Physical Journal Plus, 2017-09-01)
    The large majority of astronomical observations are based on intensity measurements as a function of either wavelength or time, or both. Polarimetry, a technique which measures the way in which the electromagnetic field associated to the radiation oscillates, does provide further information about the objects that have emitted or scattered the observed radiation. For instance, polarimetric measurements can provide important constraints to the characterisation of cosmic dust (be it of interstellar or cometary origin), of the surfaces of the atmosphereless bodies and of planetary atmospheres. This property has been exploited in solar system science to study asteroids, comets, rocky and giant gaseous planets, and their satellites. In this paper we present a review of the polarimetric studies of the small bodies of the Solar System.
  • Diagnosing transient plasma status: from solar atmosphere to tokamak divertor

    RAL Space, Science and Technology Facilities Council, Rutherford Appleton Laboratory, Harwell Oxford, Didcot OX11 0QX, U.K.; Department of Physics, University of Strathlyde, 107 Rottenrow, Glasgow G4 0NG, U.K.; Culham Centre for Fusion Energy, Culham Science Centre, Abingdon OX14 3DB, U.K.; Armagh Observatory, College Hill, Armagh BT61 9DG, U.K.; Giunta, A. S.; Henderson, S.; O'Mullane, M.; Harrison, J.; Doyle, J. G.; Summers, H. P. (Journal of Instrumentation, 2016-09-01)
    This work strongly exploits the interdisciplinary links between astrophysical (such as the solar upper atmosphere) and laboratory plasmas (such as tokamak devices) by sharing the development of a common modelling for time-dependent ionisation. This is applied to the interpretation of solar flare data observed by the UVSP (Ultraviolet Spectrometer and Polarimeter), on-board the Solar Maximum Mission and the IRIS (Interface Region Imaging Spectrograph), and also to data from B2-SOLPS (Scrape Off Layer Plasma Simulations) for MAST (Mega Ampère Spherical Tokamak) Super-X divertor upgrade. The derived atomic data, calculated in the framework of the ADAS (Atomic Data and Analysis Structure) project, allow equivalent prediction in non-stationary transport regimes and transients of both the solar atmosphere and tokamak divertors, except that the tokamak evolution is about one thousand times faster.
  • HST spectroscopy of chemically peculiar hot subdwarfs: PG 0909+276 and UVO0512-08

    Armagh Observatory and Planetarium, N. Ireland and University of Shefleld, Department of Astrophysics, Shefleld, UK; Wild, James; Jeffery, Christopher Simon (Open Astronomy, 2017-12-01)
    High-resolution ultraviolet spectroscopy of two chemically peculiar hot subdwarfs, PG 0909+276 and UVO0512-08, has been obtained using the Hubble Space Telescope. Chemical abundances in the stars' atmospheres were measured from previous optical spectra and from the new ultraviolet observations. Iron-group metals, including cobalt, copper and zinc, are highly enriched relative to typical subdwarf B (sdB) stars. Lead is also enriched, but with an abundance similar to other sdB stars. The surface chemistry of these two stars is quite distinct from both hydrogen-rich normal sdB stars and also from the intermediate helium-rich sdB stars which show heavy-element superabundances. A full explanation for exotic chemistries in hot subdwarfs remains elusive.
  • New Intense Multiband Photometric Observations of the Hot Carbon Star V348 Sagittarii (Abstract)

    Oude Bleken 12, Mol 2400, Belgium; Armagh Observatory, College Hill, Armagh BT61 9DG, United Kingdom; Hambsch, F.; Jeffery, C. S. (Journal of the American Association of Variable Star Observers (JAAVSO), 2019-06-01)
    (Abstract only) V348 Sgr is one of four hot carbon-rich and hydrogen-deficient stars. It is also the central star of a planetary nebula with a strong stellar wind, an infrared dust excess, and a circumstellar dust shell. Since July 2014, near daily multi-band photometric observations have been obtained at the Remote Observatory Atacama Desert (ROAD) close to San Pedro de Atacama, Chile. Strong variations of the brightness of V348 Sgr have been observed, ranging from magnitude 19 to 11.2 in V band. No clear periodicity is discernible in the data. The observed light curve shows much more variation and on a much shorter time scale than that of R CrB, the prototype hydrogen deficient, carbon- and helium-rich star. The star becomes markedly redder during extinction phases as a consequence of obscuring dust. The particular challenge in this case is to understand what triggers the production of dust.
  • A review of seismic observations of Kepler and K2-Observed sdBV stars

    Department of Physics, Astronomy and Materials Science, Missouri StateUniversity, United States of America; Department of Physics, Astronomy and Materials Science, Missouri StateUniversity, United States of America; Suhora Observatory and Krakow Pedagogical University,Krakow, Poland; Nordic Optical Telescope,Santa Cruz de Tenerife, Spain; Armagh Observatory and Planetarium,Armagh, Ireland; Reed, Michael D.; Baran, Andrzej S.; Telting, John H.; Østensen, Roy H.; Jeffery, Christopher S.; Kern, Joshua W.; et al. (Open Astronomy, 2018-07-01)
    This paper reviews recent seismic findings from Kepler and K2 data. Using three years of short cadence Kepler (K1) data, it is possible to examine time evolution of pulsations in an unprecedented way. While K2 observations are shorter, only three months, they are important as they are finding more sdBV stars than K1 did. Most importantly, K2 is discovering more p-mode pulsators with coverage not possible to get from the ground.
  • LS IV — 14°116 : A Time-Resolved Spectroscopic Study

    Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK. School of Physics, Trinity College Dublin, College Green, Dublin 2, Ireland; Martin, Pamela; Jeffery, C. Simon (Open Astronomy, 2017-12-01)
    LSIV-14 116 is a very unusual subdwarf B star. It pulsates non-radially with high-order g-modes, these pulsations are unexpected and unexplained, as the effective temperature is 6 000K hotter than the blue edge of the hot subdwarf g-mode instability strip. Its spectrum is enriched in helium which is not seen in either the V361 Hya (p-mode pulsators) or the V1093 Her stars (g-mode pulsators). Even more unusual is the 4 dex overabundance of zirconium, yttrium, and strontium. It is proposed that these over-abundances are a result of extreme chemical stratification driven by radiative levitation. We have over 20hrs of VLT/UVES spectroscopy from which we have obtained radial velocity curves for individual absorption lines. We are currently exploring ways in which to resolve the photospheric motion as a function of optical depth.
  • Subaru and Salt Spectroscopy of Chemically Peculiar Hot Subdwarfs

    Armagh Observatory and Planetarium, Armagh, Ireland; School of Physics, University of Hyderabad, CUC, Gachibowli, Hyderabad, Telangana 500046, India; Department of Physics, University of Nebraska at Omaha, Omaha, USA; South African Astronomical Observatory, PO Box 9, Observatory 7935, Cape Town, South Africa; Department of Physics, Astronomy andMaterials Science, Missouri State University, 901 S. National, Springfield, MO 65897, USA; Jeffery, C. Simon; Neelamkodan, Naslim; Woolf, Vincent M.; Crawford, Steven M.; Østensen, Roy H. (Open Astronomy, 2017-12-01)
    The majority of hot subdwarfs lie on or close to the helium main-sequence. Many have hydrogen-rich surfaces, but a substantial fraction of the hotter subdwarfs have hydrogen-depleted or hydrogen-deficient surfaces. Amongst the former, three were known to show extraordinary overabundances of heavy elements including zirconium and lead. Using Subaru/HDS,we commenced a high-resolution survey of hydrogen-depleted subdwarfs to discover new members of the class. UVO 0825+15, was found to exhibit strong lead lines, to be an intrinsic variable in K2 field 5, and to have a relatively high space motion. Two other lead-rich subdwarfs have been found in the Subaru sample. A much wider survey is in progress using SALT/HRS. Discoveries so far include one extreme helium star similar to V652 Her, and an intermediate helium star with possible comparison to HD144941. Analyses of the hotter and more compact members of the sample are continuing.
  • The Detection and Attribution of Northern Hemisphere Land Surface Warming (1850–2018) in Terms of Human and Natural Factors: Challenges of Inadequate Data

    Center for Environmental Research and Earth Sciences (CERES), Salem, MA 01970, USA; Institute of Earth Physics and Space Science (EPSS), H-9400 Sopron, Hungary; Center for Environmental Research and Earth Sciences (CERES), Salem, MA 01970, USA; Independent Researcher, D08 Dublin, Ireland;; Center for Environmental Research and Earth Sciences (CERES), Salem, MA 01970, USA; Independent Researcher, D08 Dublin, Ireland; International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775, USA; Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA; Independent Researcher, 211 10 Malmö, Sweden; Osservatorio Astronomico di Padova, INAF, Vicolo Osservatorio 5, 35122 Padova, Italy; Department of Physics and Astronomy, University of Padua, Via Francesco Marzolo, 8, 35131 Padova, Italy; Independent Researcher, Charlevoix, MI 49720, USA; Armagh Observatory, College Hill, Armagh BT61 9DG, UK; Comisión de Investigaciones Científicas de la Provincia de Buenos Aires, Calle 526 entre 10 y 11, La Plata 1900, Argentina; Grupo de Estudios Ambientales, Universidad Tecnológica Nacional, Colón 332, San Nicolás, Buenos Aires 2900, Argentina;; et al. (Climate, 2023-08-01)
    A statistical analysis was applied to Northern Hemisphere land surface temperatures (1850–2018) to try to identify the main drivers of the observed warming since the mid-19th century. Two different temperature estimates were considered—a rural and urban blend (that matches almost exactly with most current estimates) and a rural-only estimate. The rural and urban blend indicates a long-term warming of 0.89 °C/century since 1850, while the rural-only indicates 0.55 °C/century. This contradicts a common assumption that current thermometer-based global temperature indices are relatively unaffected by urban warming biases. Three main climatic drivers were considered, following the approaches adopted by the Intergovernmental Panel on Climate Change (IPCC)'s recent 6th Assessment Report (AR6): two natural forcings (solar and volcanic) and the composite all anthropogenic forcings combined time series recommended by IPCC AR6. The volcanic time series was that recommended by IPCC AR6. Two alternative solar forcing datasets were contrasted. One was the Total Solar Irradiance (TSI) time series that was recommended by IPCC AR6. The other TSI time series was apparently overlooked by IPCC AR6. It was found that altering the temperature estimate and/or the choice of solar forcing dataset resulted in very different conclusions as to the primary drivers of the observed warming. Our analysis focused on the Northern Hemispheric land component of global surface temperatures since this is the most data-rich component. It reveals that important challenges remain for the broader detection and attribution problem of global warming: (1) urbanization bias remains a substantial problem for the global land temperature data; (2) it is still unclear which (if any) of the many TSI time series in the literature are accurate estimates of past TSI; (3) the scientific community is not yet in a position to confidently establish whether the warming since 1850 is mostly human-caused, mostly natural, or some combination. Suggestions for how these scientific challenges might be resolved are offered.
  • Challenges in the Detection and Attribution of Northern Hemisphere Surface Temperature Trends Since 1850

    Center for Environmental Research and Earth Science (CERES), Salem, MA 01970, USA; Independent scientists, Dublin, Ireland; Center for Environmental Research and Earth Science (CERES), Salem, MA 01970, USA; Institute of Earth Physics and Space Science (EPSS), Sopron, Hungary; Retired, formerly Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA; Independent researcher, Malmö, Sweden; Retired, formerly Armagh Observatory, College Hill, Armagh BT61 9DG, Northern Ireland, UK; Comisión de Investigaciones Científicas de la Provincia de Buenos Aires, Argentina; Grupo de Estudios Ambientales, Universidad Tecnológica Nacional, Colón 332, San Nicolás (2900), Buenos Aires, Argentina; Laboratorio de Ionosfera, Atmosfera Neutra y Magnetosfera (LIANM), Facultad de Ciencias Exactas y Tecnología, Universidad Nacional de Tucumán, Av. Independencia 1800, 4000 Tucumán, Argentina; Instituto de Física del Noroeste Argentino (Consejo Nacional de Investigaciones Científicas y Técnicas-Universidad Nacional de Tucumán), 4000 Tucumán, Argentina; Faculty of Geography, Lomonosov Moscow State University, Leninskie Gory St. 1, Moscow 119991, Russia; Helmut-Schmidt-University, Hamburg, Germany; Center of Excellence in Information Systems, Tennessee State University, Nashville, TN 37209 USA; et al. (Research in Astronomy and Astrophysics, 2023-10-01)
    Since 2007, the Intergovernmental Panel on Climate Change (IPCC) has heavily relied on the comparison between global climate model hindcasts and global surface temperature (ST) estimates for concluding that post-1950s global warming is mostly human-caused. In Connolly et al., we cautioned that this approach to the detection and attribution of climate change was highly dependent on the choice of Total Solar Irradiance (TSI) and ST data sets. We compiled 16 TSI and five ST data sets and found by altering the choice of TSI or ST, one could (prematurely) conclude anything from the warming being mostly human-caused to mostly natural. Richardson and Benestad suggested our analysis was erroneous and flawed because we did not use a multilinear regression. They argued that applying a multilinear regression to one of the five ST series re-affirmed the IPCC's attribution statement. They also objected that many of the published TSI data sets were out-of-date. However, here we show that when applying multilinear regression analysis to an expanded and updated data set of 27 TSI series, the original conclusions of Connolly et al. are confirmed for all five ST data sets. Therefore, it is still unclear whether the observed warming is mostly human-caused, mostly natural or some combination of both.
  • Progress on nuclear reaction rates affecting the stellar production of <SUP>26</SUP>Al

    Department of Physics, University of York, Heslington, York, YO10 5DD, United Kingdom; Konkoly Observatory, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Konkoly Thege Miklós út 15-17, H-1121 Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Physics, Budapest 1117, Pázmány Péter sétány 1/A, Hungary; School of Physics and Astronomy, Monash University, VIC 3800, Australia; Department of Physics, University of Jyvaskyla, P.O. Box 35 (YFL), FI-40014 University of Jyvaskyla, Finland; School of Physics, University of the Witwatersrand, Johannesburg 2050, South Africa; iThemba Laboratory for Accelerator Based Sciences, Somerset West 7129, South Africa; Physics Department, University of Notre Dame, Notre Dame, IN-46556, United States of America; Konkoly Observatory, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Konkoly Thege Miklós út 15-17, H-1121 Budapest, Hungary; Graduate School of Physics, University of Szeged, Dom tér 9, Szeged, 6720 Hungary; Konkoly Observatory, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Konkoly Thege Miklós út 15-17, H-1121 Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Physics, Budapest 1117, Pázmány Péter sétány 1/A, Hungary; Joint Institute for Nuclear Astrophysics, Center for the Evolution of the Elements, Michigan State University, 640 South Shaw Lane, East Lansing, MI 48824, United States of America; NuGrid Collaboration, nugridstars.org; Department of Physics and Astronomy, Louisiana State University, Baton Rouge, LA 70803, United States of America; Max Planck Institut für extraterrestrische Physik, D-85748 Garching, Germany; Université Paris-Saclay, CNRS/IN2P3, IJCLab, F-91405 Orsay, France; et al. (Journal of Physics G Nuclear Physics, 2023-01-01)
    The radioisotope <SUP>26</SUP>Al is a key observable for nucleosynthesis in the Galaxy and the environment of the early Solar System. To properly interpret the large variety of astronomical and meteoritic data, it is crucial to understand both the nuclear reactions involved in the production of <SUP>26</SUP>Al in the relevant stellar sites and the physics of such sites. These range from the winds of low- and intermediate-mass asymptotic giant branch stars; to massive and very massive stars, both their Wolf-Rayet winds and their final core-collapse supernovae (CCSN); and the ejecta from novae, the explosions that occur on the surface of a white dwarf accreting material from a stellar companion. Several reactions affect the production of <SUP>26</SUP>Al in these astrophysical objects, including (but not limited to) <SUP>25</SUP>Mg(p, γ)<SUP>26</SUP>Al, <SUP>26</SUP>Al(p, γ)<SUP>27</SUP>Si, and <SUP>26</SUP>Al(n, p/α). Extensive experimental effort has been spent during recent years to improve our understanding of such key reactions. Here we present a summary of the astrophysical motivation for the study of <SUP>26</SUP>Al, a review of its production in the different stellar sites, and a timely evaluation of the currently available nuclear data. We also provide recommendations for the nuclear input into stellar models and suggest relevant, future experimental work.
  • Multiwavelength High-resolution Observations of Chromospheric Swirls in the Quiet Sun

    Centre of Fusion, Space and Astrophysics, University of Warwick, Coventry CV4 7AL, UK; ASI—Italian Space Agency, Via del Politecnico snc, Rome, Italy ; INAF-OAR National Institute for Astrophysics, I-00078 Monte Porzio Catone (RM), Italy; High Altitude Observatory, National Center for Atmospheric Research, P.O. Box 3000, Boulder CO 80307-3000, USA; Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK; Department of Mathematics &amp; Information Sciences, Northumbria University, Newcastle Upon Tyne, NE1 8ST, UK; Institute of Theoretical Astrophysics, University of Oslo, P.O. Box 1029 Blindern, NO-0315, Oslo, Norway ; Rosseland Centre for Solar Physics, University of Oslo, P.O. Box 1029 Blindern, NO-0315, Oslo, Norway; Shetye, Juie; Verwichte, Erwin; Stangalini, Marco; Judge, Philip G.; et al. (The Astrophysical Journal, 2019-08-01)
    We report observations of small-scale swirls seen in the solar chromosphere. They are typically 2 Mm in diameter and last around 10 minutes. Using spectropolarimetric observations obtained by the CRisp Imaging Spectro-Polarimeter at the Swedish 1 m Solar Telescope, we identify and study a set of swirls in chromospheric Ca II 8542 Å and Hα lines as well as in the photospheric Fe I line. We have three main areas of focus. First, we compare the appearance, morphology, dynamics, and associated plasma parameters between the Ca II and Hα channels. Rotation and expansion of the chromospheric swirl pattern are explored using polar plots. Second, we explore the connection to underlying photospheric magnetic concentration (MC) dynamics. MCs are tracked using the SWAMIS tracking code. The swirl center and MC remain cospatial and share similar periods of rotation. Third, we elucidate the role swirls play in modifying chromospheric acoustic oscillations and found a temporary reduction in wave period during swirls. We use cross-correlation wavelets to examine the change in period and phase relations between different wavelengths. The physical picture that emerges is that a swirl is a flux tube that extends above an MC in a downdraft region in an intergranular lane. The rotational motion of the MC matches the chromospheric signatures. We could not determine whether a swirl is a gradual response to the photospheric motion or an actual propagating Alfvénic wave.
  • Photospheric Observations of Surface and Body Modes in Solar Magnetic Pores

    Astrophysics Research Centre, School of Mathematics and Physics, Queen's University Belfast, Belfast, BT7 1NN, UK ; Solar Physics and Space Plasma Research Centre (SP2RC), University of Sheffield, Hicks Building, Hounsfield Road, Sheffield, S3 7RH, UK;; Mathematics and Information Sciences, Northumbria University, Newcastle Upon Tyne, NE1 8ST, UK; Astrophysics Research Centre, School of Mathematics and Physics, Queen's University, Belfast, BT7 1NN, UK ; Department of Physics and Astronomy, California State University Northridge, Northridge, CA 91330, USA; Solar Physics and Space Plasma Research Centre (SP2RC), University of Sheffield, Hicks Building, Hounsfield Road, Sheffield, S3 7RH, UK; Astrophysics Research Centre, School of Mathematics and Physics, Queen's University, Belfast, BT7 1NN, UK; School of Mathematics and Statistics, University of St Andrews, St Andrews, KY16 9SS, UK; Armagh Observatory &amp; Planetarium, College Hill, Armagh, BT61 9DG, UK; Department of Physics and Astronomy, California State University Northridge, Northridge, CA 91330, USA; Solar Physics and Space Plasma Research Centre (SP2RC), University of Sheffield, Hicks Building, Hounsfield Road, Sheffield, S3 7RH, UK; Debrecen Heliophysical Observatory (DHO), Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, 4010 Debrecen, P.O. Box 30, Hungary; Keys, Peter H.; et al. (The Astrophysical Journal, 2018-04-01)
    Over the past number of years, great strides have been made in identifying the various low-order magnetohydrodynamic wave modes observable in a number of magnetic structures found within the solar atmosphere. However, one aspect of these modes that has remained elusive, until now, is their designation as either surface or body modes. This property has significant implications for how these modes transfer energy from the waveguide to the surrounding plasma. Here, for the first time to our knowledge, we present conclusive, direct evidence of these wave characteristics in numerous pores that were observed to support sausage modes. As well as outlining methods to detect these modes in observations, we make estimates of the energies associated with each mode. We find surface modes more frequently in the data, as well as that surface modes appear to carry more energy than those displaying signatures of body modes. We find frequencies in the range of ∼2-12 mHz, with body modes as high as 11 mHz, but we do not find surface modes above 10 mHz. It is expected that the techniques we have applied will help researchers search for surface and body signatures in other modes and in differing structures from those presented here.
  • Polarimetric view of the changing type Seyfert galaxy ESO 362-G018.

    Centro de Astrobiología (CSIC-INTA), Dep. de Astrofíica, Villanueva de la Cañada, E-28692, Madrid, Spain; Armagh Observatory, College Hill, Armagh BT61 9 DG, UK; Institut d'Astrophysique et de Géophysique, Université de Liége, Allée du 6 Août 19c, B5c, 4000 Liége, Belgium; Agís-González, B.; Bagnulo, S.; Hutsemékers, D.; Montesinos, B.; Miniutti, G.; Sanfrutos, M. (Highlights on Spanish Astrophysics IX, 2017-03-01)
    ESO362-G018 is an active galactic nucleus (AGN) which is classified as a Seyfert 1.5 galaxy e.g. by Bennert et al. (2006), (black data set on figure 1). However, Parisi et. al (2009) found an optical spectrum of this source which was taken during the 6dF Galaxy Survey, but it does not show the broad Balmer lines required to classify it as Seyfert 1 galaxy (red data set on figure 1). On the other hand, the results obtained by Agis-Gonzalez et al. (2014❩ in a X-ray analysis of this same source reveal that the inclination of ESO362- G018 i = 53° ± 5° is consistent with the picture of an AGN looked through the upper layers of a clumpy, dusty torus. Thus, according to the Unification Models of AGN and the clumpy nature of the torus, our interpretation of the different spectra is the following one. On 30th of January of 2003 (when the spectrum belonging to the 6dF survey was obtained), our line of sight intercepted a (or several aligned) torus clump(s) with much greater column density than its environment. Accordingly, the nucleus and the broad line region (❨BLR)❩ would be obscured. This allowed only the narrow emission lines to emerge from the narrow line region (NRL). Otherwise, on 18th of September of 2004 (when the spectrum by Bennert et al. 2006 was obtained) there is no clump to intercept and the BLR is not obscured so that the broad Balmer emission lines could be detected.
  • TESS Photometry of AM Her and AR UMa: Binary Parameters, Cyclotron Emission Modeling, and Mass Transfer Duty Cycles

    New Mexico State University, MSC 3DA, Las Cruces, NM 88003, USA; Picture Rocks Observatory, 1025 S. Solano Dr. Suite D., Las Cruces, NM 88001, USA; Finnish Centre for Astronomy with ESO, Quantum, Vesilinnantie 5, FI-20014, University of Turku, Finland; Mullard Space Science Laboratory, University College London, Holmbury St. Mary, Surrey RH5 6NT, UK; Department of Physics, The George Washington University, Washington, DC 20052, USA; Centre for Extragalactic Astronomy, Department of Physics, Durham University, South Road, Durham DH1 3LE, UK; Astronomical Observatory, University of Warsaw, Al. Ujazdowskie 4, 00-478 Warsaw, Poland; Bay Area Environmental Research Institute, Moffett Field, CA 94035, USA; Picture Rocks Observatory, 1025 S. Solano Dr. Suite D., Las Cruces, NM 88001, USA; Instituto Nacional de Pesquisas Espaciais, Av. dos Astronautas 1758, São José dos Campos, SP 12227-010, Brazil; Department of Physics, University of Notre Dame, Notre Dame, IN 46556, USA; Department of Astronomy, University of Washington, Seattle, WA 98195, USA; et al. (The Astrophysical Journal, 2024-04-01)
    Transiting Exoplanet Survey Satellite (TESS) photometry of the polars AM Herculis (AM Her) and AR Ursae Majoris (AR UMa) is presented, along with high-speed photometry. AM Her shows a variety of high states with frequent transitions between them. TESS photometry of AR UMa in the low state reveals no evidence of accretion, while the McDonald 2.1 m telescope caught AR UMa in its high accretion state. Roche-lobe overflow is shut off during low states of AR UMa, while accretion often still takes place during low states of AM Her. We derive inclinations of 50° and 70° for AM Her and AR UMa respectively. To model the high-state light curves of AM Her, we employ a self-organized map light-curve classification scheme to establish common accretion configurations. The cyclotron radiation properties then allow the production of emission region maps on the surface of the white dwarf. The accretion geometry of AM Her is most consistent with a multipolar field structure. The high-state photometry of AR UMa has stochastic accretion flaring, which we attribute to magnetically buffeted mass transfer through the inner Lagrangian point L1. To consider this possibility, we examine the magnetism of both stars and argue that the local magnetic field near L1 can initiate short-lived accretion events and affect transitions between high and low accretion states in both AM Her and AR UMa. In particular, AR UMa has the low state as its default, while AM Her and most other active polars are in the high state by default.
  • Orbital Modification of the Himalia Family during an Early Solar System Dynamical Instability

    dli@arm.ac.uk; Armagh Observatory and Planetarium College Hill, Armagh, BT61 9DG, UK; School of Mathematics and Physics, Queen's University Belfast University Road, Belfast, BT7 1NN, UK; ;; Armagh Observatory and Planetarium College Hill, Armagh, BT61 9DG, UK; Li, Daohai; Christou, Apostolos A. (The Astronomical Journal, 2017-11-01)
    Among the irregular satellites orbiting Jupiter, the Himalia family is characterized by a high velocity dispersion δ v of several hundred ms<SUP>-1</SUP> among its members, inconsistent with a collisional origin. Efforts to account for this through internecine gravitational interactions do not readily reproduce this feature. Here, we revisit the problem in the context of recent cosmogonical models, where the giant planets migrated significantly through interaction with a planetesimal disk and suffered encounters with planetesimals and planet-sized objects. Our starting assumption is that family formation either predated this phase or occurred soon after its onset. We simulate numerically the diffusive effect of three distinct populations of perturbers on a set of test particles representing the family: Moon-sized (MPT) and Pluto-sized (PPT) planetesimals, and planetary-mass objects (PMO) with masses typical of ice-giant planets. We find that PPT flybys are inefficient, but encounters with MPTs raise the δ v of ∼60% of our test particles to &gt; 200 ms<SUP>-1</SUP> with respect to Himalia, in agreement with observations. As MPTs may not have been abundant in the disk, we simulate encounters between Jupiter and PMOs. We find that too few encounters generate less dispersion than MPTs while too many essentially destroy the family. For PMO masses in the range 5-20 m<SUB>\oplus</SUB>, the family orbital distribution is reproduced by a few tens of encounters.
  • New Evidence for a Physical Link between Asteroids (155140) 2005 UD and (3200) Phaethon

    Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff, AZ 86001, USA; Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland; Department of Astronomy &amp; Planetary Science, Northern Arizona University, P.O. Box 6010, Flagstaff, AZ 86011, USA; Las Cumbres Observatory, CA, USA; Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK; Institute of Astronomy and National Astronomical Observatory, Bulgarian Academy of Sciences, 72, Tsarigradsko Chaussèe Blvd., Sofia BG-1784, Bulgaria; Aerospace Engineering, Nihon University, 7-24-1 Narashinodai, Funabashi, Chiba 2748501, Japan; Planetary Exploration Research Center, Chiba Institute of Technology, Narashino, Japan; Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland; Astrophysics Research Centre, School of Mathematics and Physics, Queen's University Belfast, Belfast BT7 1NN, UK; Space sciences, Technologies &amp; Astrophysics Research (STAR) Institute University of Liège Allée du 6 Août 19, B-4000 Liège, Belgium; Aix Marseille Université, CNRS, LAM (Laboratoire d'Astrophysique de Marseille) UMR 7326, F-13388, Marseille, France; Space sciences, Technologies, France; Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland; Division of Space Technology, Luleå University of Technology, Box 848, SE-98128 Kiruna, Sweden; et al. (The Planetary Science Journal, 2020-06-01)
    In 2018, the near-Earth object (155140) 2005 UD (hereafter UD) experienced a close fly by of the Earth. We present results from an observational campaign involving photometric, spectroscopic, and polarimetric observations carried out across a wide range of phase angles (0°7-88°). We also analyze archival NEOWISE observations. We report an absolute magnitude of H<SUB>V</SUB> = 17.51 ± 0.02 mag and an albedo of p<SUB>V</SUB> = 0.10 ± 0.02. UD has been dynamically linked to Phaethon due their similar orbital configurations. Assuming similar surface properties, we derived new estimates for the diameters of Phaethon and UD of D = 5.4 ± 0.5 km and D = 1.3 ± 0.1 km, respectively. Thermophysical modeling of NEOWISE data suggests a surface thermal inertia of ${\rm{\Gamma }}={300}_{-110}^{+120}$ and regolith grain size in the range of 0.9-10 mm for UD and grain sizes of 3-30 mm for Phaethon. The light curve of UD displays a symmetric shape with a reduced amplitude of Am(0) = 0.29 mag and increasing at a linear rate of 0.017 mag/° between phase angles of 0° and ∼25°. Little variation in light-curve morphology was observed throughout the apparition. Using light-curve inversion techniques, we obtained a sidereal rotation period P = 5.235 ± 0.005 hr. A search for rotational variation in spectroscopic and polarimetric properties yielded negative results within observational uncertainties of ∼10% μm<SUP>-1</SUP> and ∼16%, respectively. In this work, we present new evidence that Phaethon and UD are similar in composition and surface properties, strengthening the arguments for a genetic relationship between these two objects. <SUP>*</SUP> Partially based on data collected with 2 m RCC telescope at Rozhen National Astronomical Observatory.
  • Can a robot be a scientist? Developing students' epistemic insight through a lesson exploring the role of human creativity in astronomy

    LASAR Research Centre, Canterbury Christ Church University, North Holmes Road, Canterbury, CT1 1QU; Simon Langton Grammar School for Boys, Langton Lane, Canterbury CT47AS; Armagh Observatory, College Hill, Armagh BT619DM; Billingsley, Berry; Heyes, Joshua M.; Lesworth, Tim; Sarzi, Marc (Physics Education, 2023-01-01)
    Artificial intelligence is transforming the practice of science worldwide. Breakthroughs in machine learning are enabling, for example, the discovery of potentially habitable exoplanets beyond our solar system. The growing role of artificial intelligence (AI) in science raises questions for scientists, philosophers, computer scientists … and educators. How will the scholarship and practice of science education respond to the growing role of artificial intelligence in science? Questions like 'Can a robot be a scientist?' can help stimulate students' epistemic curiosity, about the nature of scientific knowledge, including the value and importance of apparently uniquely human attributes such as creativity. In this article we explain the development and delivery of a science lesson using the question 'can a robot be a scientist?' to explore the role of human creativity in scientific observation and classification, using resources and activities created for the citizen scientist project 'Galaxy Zoo'.

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