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  • 2015-2019  (3)
  • 1
    Publikationsdatum: 2015-06-26
    Beschreibung: Exoplanets orbiting close to their parent stars may lose some fraction of their atmospheres because of the extreme irradiation. Atmospheric mass loss primarily affects low-mass exoplanets, leading to the suggestion that hot rocky planets might have begun as Neptune-like, but subsequently lost all of their atmospheres; however, no confident measurements have hitherto been available. The signature of this loss could be observed in the ultraviolet spectrum, when the planet and its escaping atmosphere transit the star, giving rise to deeper and longer transit signatures than in the optical spectrum. Here we report that in the ultraviolet the Neptune-mass exoplanet GJ 436b (also known as Gliese 436b) has transit depths of 56.3 +/- 3.5% (1sigma), far beyond the 0.69% optical transit depth. The ultraviolet transits repeatedly start about two hours before, and end more than three hours after the approximately one hour optical transit, which is substantially different from one previous claim (based on an inaccurate ephemeris). We infer from this that the planet is surrounded and trailed by a large exospheric cloud composed mainly of hydrogen atoms. We estimate a mass-loss rate in the range of about 10(8)-10(9) grams per second, which is far too small to deplete the atmosphere of a Neptune-like planet in the lifetime of the parent star, but would have been much greater in the past.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ehrenreich, David -- Bourrier, Vincent -- Wheatley, Peter J -- des Etangs, Alain Lecavelier -- Hebrard, Guillaume -- Udry, Stephane -- Bonfils, Xavier -- Delfosse, Xavier -- Desert, Jean-Michel -- Sing, David K -- Vidal-Madjar, Alfred -- England -- Nature. 2015 Jun 25;522(7557):459-61. doi: 10.1038/nature14501.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Observatoire de l'Universite de Geneve, 51 chemin des Maillettes, 1290 Versoix, Switzerland. ; Department of Physics, University of Warwick, Coventry CV4 7AL, UK. ; 1] CNRS, UMR 7095, Institut d'Astrophysique de Paris, 98 bis boulevard Arago, 75014 Paris, France [2] Sorbonnes Universites, UPMC Univ. Paris 6, UMR 7095, Institut d'Astrophysique de Paris, 98 bis boulevard Arago, 75014 Paris, France. ; 1] CNRS, UMR 7095, Institut d'Astrophysique de Paris, 98 bis boulevard Arago, 75014 Paris, France [2] Sorbonnes Universites, UPMC Univ. Paris 6, UMR 7095, Institut d'Astrophysique de Paris, 98 bis boulevard Arago, 75014 Paris, France [3] Observatoire de Haute-Provence, CNRS &OAMP, 04870 Saint-Michel-l'Observatoire, France. ; 1] Univ. Grenoble Alpes, IPAG, F-38000 Grenoble, France [2] CNRS, IPAG, F-38000 Grenoble, France. ; CASA, Department of Astrophysical &Planetary Sciences, University of Colorado, 389-UCB, Boulder, Colorado 80309, USA. ; Astrophysics Group, School of Physics, University of Exeter, Stocker Road, Exeter EX4 4QL, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26108854" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Digitale ISSN: 1476-4687
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2015-12-18
    Beschreibung: Thousands of transiting exoplanets have been discovered, but spectral analysis of their atmospheres has so far been dominated by a small number of exoplanets and data spanning relatively narrow wavelength ranges (such as 1.1-1.7 micrometres). Recent studies show that some hot-Jupiter exoplanets have much weaker water absorption features in their near-infrared spectra than predicted. The low amplitude of water signatures could be explained by very low water abundances, which may be a sign that water was depleted in the protoplanetary disk at the planet's formation location, but it is unclear whether this level of depletion can actually occur. Alternatively, these weak signals could be the result of obscuration by clouds or hazes, as found in some optical spectra. Here we report results from a comparative study of ten hot Jupiters covering the wavelength range 0.3-5 micrometres, which allows us to resolve both the optical scattering and infrared molecular absorption spectroscopically. Our results reveal a diverse group of hot Jupiters that exhibit a continuum from clear to cloudy atmospheres. We find that the difference between the planetary radius measured at optical and infrared wavelengths is an effective metric for distinguishing different atmosphere types. The difference correlates with the spectral strength of water, so that strong water absorption lines are seen in clear-atmosphere planets and the weakest features are associated with clouds and hazes. This result strongly suggests that primordial water depletion during formation is unlikely and that clouds and hazes are the cause of weaker spectral signatures.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sing, David K -- Fortney, Jonathan J -- Nikolov, Nikolay -- Wakeford, Hannah R -- Kataria, Tiffany -- Evans, Thomas M -- Aigrain, Suzanne -- Ballester, Gilda E -- Burrows, Adam S -- Deming, Drake -- Desert, Jean-Michel -- Gibson, Neale P -- Henry, Gregory W -- Huitson, Catherine M -- Knutson, Heather A -- des Etangs, Alain Lecavelier -- Pont, Frederic -- Showman, Adam P -- Vidal-Madjar, Alfred -- Williamson, Michael H -- Wilson, Paul A -- England -- Nature. 2016 Jan 7;529(7584):59-62. doi: 10.1038/nature16068. Epub 2015 Dec 14.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Astrophysics Group, School of Physics, University of Exeter, Stocker Road, Exeter EX4 4QL, UK. ; Department of Astronomy and Astrophysics, University of California, Santa Cruz, California 95064, USA. ; Department of Physics, University of Oxford, Keble Road, Oxford OX1 3RH, UK. ; Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721, USA. ; Department of Astrophysical Sciences, Peyton Hall, Princeton University, Princeton, New Jersey 08544, USA. ; Department of Astronomy, University of Maryland, College Park, Maryland 20742, USA. ; Department of Astrophysical and Planetary Sciences, University of Colorado, Boulder, Colorado 80309, USA. ; European Southern Observatory, Karl-Schwarzschild-Strasse 2, D-85748 Garching bei Munchen, Germany. ; Center of Excellence in Information Systems, Tennessee State University, Nashville, Tennessee 37209, USA. ; Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA. ; CNRS, Institut dAstrophysique de Paris, UMR 7095, 98 bis boulevard Arago, 75014 Paris, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26675732" target="_blank"〉PubMed〈/a〉
    Schlagwort(e): Atmosphere/*chemistry ; Extraterrestrial Environment/*chemistry ; Jupiter ; *Planets ; Pressure ; Spectrophotometry, Infrared ; Telescopes ; Temperature ; Water/*analysis
    Print ISSN: 0028-0836
    Digitale ISSN: 1476-4687
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2015-04-17
    Beschreibung: We present the detection of potassium in the atmosphere of HAT-P-1b using optical transit narrow-band photometry. The results are obtained using the 10.4-m Gran Telescopio Canarias together with the OSIRIS instrument in tunable filter imaging mode. We observed four transits, two at continuum wavelengths outside the potassium feature, at 6792 and 8844 Å, and two probing the potassium feature in the line wing at 7582.0 Å and the line core at 7664.9 Å using a 12 Å filter width ( R  ~ 650). The planet-to-star radius ratios in the continuum are found to be R pl / R * = 0.1176 ± 0.0013 at 6792 Å and R pl / R * = 0.1168 ± 0.0022 at 8844 Å, significantly lower than the two observations in the potassium line: R pl / R * = 0.1248 ± 0.0014 in the line wing at 7582.0 Å and R pl / R * = 0.1268 ± 0.0012 in the line core at 7664.9 Å. With a weighted mean of the observations outside the potassium feature R pl / R * = 0.1174 ± 0.0010, the potassium is detected as an increase in the radius ratio of R pl / R * = 0.0073 ± 0.0017 at 7582.0 Å and R pl / R * = 0.0094 ± 0.0016 at 7664.9 Å (a significance of 4.3 and 6.1, respectively). We hypothesize that the strong detection of potassium is caused by a large scaleheight, which can be explained by a high temperature at the base of the upper atmosphere. A lower mean molecular mass caused by the dissociation of molecular hydrogen into atomic hydrogen by the extreme ultraviolet flux from the host star may also partly explain the amplitude of our detection.
    Print ISSN: 0035-8711
    Digitale ISSN: 1365-2966
    Thema: Physik
    Publiziert von Oxford University Press
    Standort Signatur Einschränkungen Verfügbarkeit
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