Pluto’s atmosphere from the 29 June 2015 ground-based stellar occultation at the time of the New Horizons flyby
Author
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Sicardy, B.
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Talbot, J.
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Meza, E.
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Camargo, J. I. B.
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Desmars, J.
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Gault, D.
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Herald, D.
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Kerr, S.
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Pavlov, H.
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Braga Ribas, F.
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Assafin, M.
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Benedetti Rossi, G.
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Días Oliveira, A.
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Gomes Junior, A. R.
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Vieira Martins, R.
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Bérard, D.
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Kervella, Pierre
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Lecacheux, J.
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Lellouch, E.
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Beisker, W.
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Dunham, D.
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Jelínek, M.
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Duffard, R.
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Ortiz, J. L.
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Castro Tirado, A. J.
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Cunniffe, R.
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Querel, R.
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Yock, P. C.
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Cole, A. A.
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Giles, A. B.
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Hill, K. M.
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Beaulieu, J. P.
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Harnisch, M.
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Jansen, R.
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Pennell, A.
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Todd, S.
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Allen, W. H.
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Graham, P. B.
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Loader, B.
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McKay, G.
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Milner, J.
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Parker, S.
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Barry, M. A.
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Bradshaw, J.
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Broughton, J.
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Davis, L.
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Devillepoix, H.
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Drummond, J.
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Field, L.
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Forbes, M.
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Giles, D.
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Glassey, R.
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Groom, R.
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Hooper, D.
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Horvat, R.
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Hudson, G.
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Idaczyk, R.
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Jenke, D.
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Lade, B.
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Newman, J.
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Nosworthy, P.
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Purcell, P.
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Skilton, P. F.
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Streamer, M.
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Unwin, M.
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Watanabe, H.
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White, G. L.
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Watson, D.
Admission date
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2016-07-01T19:39:56Z
Available date
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2016-07-01T19:39:56Z
Publication date
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2016
Cita de ítem
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The Astrophysical Journal Letters, Volume 819, Number 2 (2016)
en_US
Identifier
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DOI http://dx.doi.org/10.3847/2041-8205/819/2/L38
Identifier
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https://repositorio.uchile.cl/handle/2250/139374
Abstract
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We present results from a multi-chord Pluto stellar occultation observed on
29 June 2015 from New Zealand and Australia. This occurred only two weeks
before the NASA New Horizons flyby of the Pluto system and serves as a useful
comparison between ground-based and space results. We find that Pluto’s atmosphere
is still expanding, with a significant pressure increase of 5±2% since
2013 and a factor of almost three since 1988. This trend rules out, as of today,
an atmospheric collapse associated with Pluto’s recession from the Sun. A central
flash, a rare occurrence, was observed from several sites in New Zealand.
The flash shape and amplitude are compatible with a spherical and transparent
atmospheric layer of roughly 3 km in thickness whose base lies at about 4 km
above Pluto’s surface, and where an average thermal gradient of about 5 K km−1
prevails. We discuss the possibility that small departures between the observed
and modeled flash are caused by local topographic features (mountains) along
Pluto’s limb that block the stellar light. Finally, using two possible temperature
profiles, and extrapolating our pressure profile from our deepest accessible level
down to the surface, we obtain a possible range of 11.9-13.7 μbar for the surface
pressure.